Foliated cataclasite, normal fault, Sasso Rosso, Italy<\/p>\n
Photo by R. Carosi, University of Torino<\/p>\n
Calcite-filled, dextral tension gashes in limestone, Elba Island (Italy)<\/p>\n
<\/a>New mailCopTensio gashes, Elba Island<\/button><\/textarea><\/p>\n<\/div>\n<\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div>Photo by R Carosi, University of Torino<\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div><\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div><\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p>New mail<textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div><\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/div>\n<\/div>\n<div><img \/><\/div>\n","modified":"2021-02-03T21:11:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2021\/01\/tension-gashes-768x575.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7923","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7923&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/tension-gashes-elba-island\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.275078291452,42.818120716576]}},{"type":"Feature","properties":{"id":7913,"name":"High temperture shear zone in migmatites","description":"<p>High temperture shear zone in Carbonifeorus migmatites of Asinara Island, Italy.<\/p>\n<p>Photo by R Carosi, University of Torino<\/p>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div><\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p>New <textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p>New mail<textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>N<textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/div>\n<\/div>\n","modified":"2021-01-15T17:50:46","color":"","icon":"","noDetails":false,"noInteraction":false,"imageGallery":[{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2021\/01\/HT-shear-zone-migmatiti-Asinara.jpg","id":7911,"caption":""}],"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2021\/01\/HT-shear-zone-migmatiti-Asinara.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7913","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7913&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/high-temperture-shear-zone-in-migmatites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.3197935701803,41.115773608307]}},{"type":"Feature","properties":{"id":7611,"name":"Danian redbeds and calciturbidites","description":"<p>Danian (early Paleocene) red hemipelagic sediments with white calciturbidites of the Cugnan Formation; Photo by Edoardo Dallanave<\/p>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/div>\n<\/div>\n<div><img \/><\/div>\n","modified":"2020-09-02T10:46:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_2536-1024x683.jpeg","accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7611","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7611&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/danian-redbeds-and-calciturbidites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[12.146285996216,46.037696361841]}},{"type":"Feature","properties":{"id":7700,"name":"Insubric Line (\u201cTonale Line\u201d) mylonites with pseudotachylyte injections","description":"<p><em><strong>Insubric Line (\u201cTonale Line\u201d) mylonites with <\/strong><\/em><strong>pseudotachylyte injections <\/strong>involving southalpine basement (“APX” : garnet, biotite, chlorite micaschists – \u201cEdolo Schists\u201d – “Scisti di Edolo” Auct. p.p., in Malonno Sheet CARG project legend, Aprica Tectonometamorphic Unit), by Torre de Li Beli Miri tower, Teglio, Sondrio province, Valtellina valley, Rhetic Alps, central Alps, Lombardy.<\/p>\n<p>(Photo: Lorusso Angelo)<\/p>\n<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-7702\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-17-Teglio-Outcropedia-1-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-17-Teglio-Outcropedia-1-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-17-Teglio-Outcropedia-1-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-17-Teglio-Outcropedia-1-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-17-Teglio-Outcropedia-1.jpg 960w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><img loading=\"lazy\" class=\"alignnone size-medium wp-image-7703\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-23-Teglio-Outcropedia-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-23-Teglio-Outcropedia-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-23-Teglio-Outcropedia-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-23-Teglio-Outcropedia-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-23-Teglio-Outcropedia.jpg 960w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/p>\n","modified":"2020-08-29T17:49:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/milon-Linea-Ins-zona-Torre-17-Teglio-Outcropedia-1-768x576.jpg","taxonomy":{"webmapp_category":[224,234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7700","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7700&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/insubric-line-tonale-line-mylonites-with-pseudotachylyte-injections\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.066189912272,46.170469734864]}},{"type":"Feature","properties":{"id":7686,"name":"Thrust Zermatt-Saas unit over Monte Rosa nappe","description":"<p>Highlight on the thrust (folded) bringing Zermatt-Saas unit (metaoceanic, amphibolites with eclogitic relics, ex basaltic tholeiitic affinity) over Monte Rosa nappe (variscan metacontinental litosphere, Brianzonese – Pennidic domain,\u00a0paragneiss with granatiferous micaschists). By the contact you can see metasomatic effects with amphibole rocks (“actinolite-tremolite series” – “tremolititi” auct.), talc and chlorites. From east sector of Corno Camoscio (Stolemberg area), next to (ex) “Citt\u00e0 di Vigevano” refugee, under Passo dei Salati (Salati pass), about 3000m asl, Gressoney valley – Sesia valley\u00a0watershed, <em>Pennine Alps, northwestern Alps. (Personal photo: Lorusso Angelo).<\/em><\/p>\n<p> <\/p>\n","modified":"2020-08-23T21:42:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/thrust-ZS-MR-Cno.Camoscio-Stolemberg-area-P.ssoSalati-MIA-768x576.jpg","taxonomy":{"webmapp_category":[234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7686","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7686&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/thrust-zermatt-saas-unit-over-monte-rosa-nappe\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.8722733531318,45.87162827204]}},{"type":"Feature","properties":{"id":7659,"name":"Permian evaporite rocks of the Bellerophon Formation pushed upward trough the nucleus of a diapiric anticline. (Dolomites, Southern Alps)","description":"<p>Photo by Marcello Lancietti:<\/p>\n<p>salt diapir by ‘Roisc dal Giaf’ – upper San Nicol\u00f2 valley – Val di Fassa<\/p>\n<p> <\/p>\n<p><img loading=\"lazy\" class=\"wp-image-7660 alignright\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/Giaf-225x300.jpg\" alt=\"\" width=\"714\" height=\"952\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/Giaf-225x300.jpg 225w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/Giaf-768x1024.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/Giaf-1152x1536.jpg 1152w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/Giaf-1536x2048.jpg 1536w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/Giaf-1080x1440.jpg 1080w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/Giaf-scaled.jpg 1920w\" sizes=\"(max-width: 714px) 100vw, 714px\" \/><\/p>\n","modified":"2020-08-23T21:36:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/Giaf-768x1024.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7659","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7659&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/permian-evaporite-rocks-of-the-bellerophon-formation-pushed-upward-trough-the-nucleus-of-a-diapiric-anticline-dolomites-southern-alps\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"museo.monzoni@rolmail.net","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.785297692297,46.424036207415]}},{"type":"Feature","properties":{"id":7635,"name":"Large-scale interference pattern by intersection of two orthogonal fold-and-thrust structural trends. (Dolomites, Southern Alps)","description":"<p>The Marmolada-Vernel thrust system superimposed on the Contrin-San Nicol\u00f2-Lagusel diapiric anticline visible in cross-section.<br \/>\nThrusting is consistent with Paleogene alpine orogenetic compressions directed toward the observer (SW). The diapiric nucleus and ladinian magmatic dikes cutting the folded beds suggest a middle Triassic age for the ENE-WSW trending fold.<\/p>\n<p>Photo by Marcello Lancietti<\/p>\n","modified":"2020-08-23T21:36:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/Marmolada_thrust--1024x635.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7635","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7635&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/large-scale-interference-pattern-by-intersection-of-two-orthogonal-fold-and-thrust-structural-trends-dolomites-southern-alps\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"museo.monzoni@rolmail.net","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.819587548038,46.436733956128]}},{"type":"Feature","properties":{"id":7637,"name":"Intersection of two orthogonal fold-and-thrust structural trends. (Dolomites, Southern Alps)","description":"<p>A big, complex fold crosscut by two transversal valleys (San Nicol\u00f2 V. and Contrin V.) dips under the Marmolada massif. Here’s the section in between with the central-upper part removed by erosion. The axial surface – striking ENE-WSW \u2013 is approximately normal to the picture’s plane and runs trough the salt diapir in the center. Passo San Nicol\u00f2 ridge, connecting Sas de Roces and Col Ombert on the opposite flanks of this diapiric anticline, is the hinge line of a perpendicular fold, sub-parallel to the Marmolada overthrust in background.<\/p>\n<p>Photo by Marcello Lancietti<\/p>\n<p><img loading=\"lazy\" class=\"alignnone wp-image-7642\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/diapiric_anticline-300x167.jpg\" alt=\"\" width=\"711\" height=\"396\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/diapiric_anticline-300x167.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/diapiric_anticline-1024x571.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/diapiric_anticline-768x429.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/diapiric_anticline-1536x857.jpg 1536w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/diapiric_anticline-2048x1143.jpg 2048w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/diapiric_anticline-1080x603.jpg 1080w\" sizes=\"(max-width: 711px) 100vw, 711px\" \/><\/p>\n","modified":"2020-08-23T21:36:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/08\/diapiric_anticline-1024x571.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7637","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7637&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/intersection-of-two-orthogonal-fold-and-thrust-structural-trends-dolomites-southern-alps\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[11.788941909494,46.42504742183]}},{"type":"Feature","properties":{"id":7615,"name":"Alagua – Stockwork of tremolite\u2013calcite veins in Teggiolo metasediments","description":"<div id=\"attachment_7616\" style=\"width: 310px\" class=\"wp-caption alignnone\"><img aria-describedby=\"caption-attachment-7616\" loading=\"lazy\" class=\"size-medium wp-image-7616\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_07-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_07-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_07-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_07-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_07-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_07-1080x810.jpg 1080w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_07.jpg 1417w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-7616\" class=\"wp-caption-text\">General view of the<br \/>stockwork of tremolite\u2013calcite<br \/>veins in Teggiolo<br \/>metasediments (46.196817 8.341331 )<\/p><\/div>\n<div id=\"attachment_7617\" style=\"width: 310px\" class=\"wp-caption alignnone\"><img aria-describedby=\"caption-attachment-7617\" loading=\"lazy\" class=\"size-medium wp-image-7617\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_08-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_08-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_08-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_08-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_08-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_08-1080x810.jpg 1080w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_08.jpg 1417w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-7617\" class=\"wp-caption-text\">close up view<\/p><\/div>\n<p>Photo by Michele Sapigni<\/p>\n<p> <\/p>\n<p> <\/p>\n","modified":"2021-02-09T16:21:54","color":"","icon":"","noDetails":false,"noInteraction":false,"zindex":"","imageGallery":[{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_07-1024x768.jpg","id":7616,"caption":"General view of the\nstockwork of tremolite\u2013calcite\nveins in Te`ggiolo\nmetasediments"},{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_08-1024x768.jpg","id":7617,"caption":"close up view"}],"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/Fig_2_07-1024x768.jpg","taxonomy":{"webmapp_category":[224]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7615","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7615&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/alagua-stockwork-of-tremolite-calcite-veins-in-teggiolo-metasediments\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.3413041779099,46.196809573679]}},{"type":"Feature","properties":{"id":7598,"name":"Sheath folds in mylonitic marble","description":"<p><img loading=\"lazy\" class=\"size-full wp-image-7599\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-scaled.jpg\" alt=\"\" width=\"2560\" height=\"1920\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-scaled.jpg 2560w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-1536x1152.jpg 1536w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-2048x1536.jpg 2048w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-1080x810.jpg 1080w\" sizes=\"(max-width: 2560px) 100vw, 2560px\" \/><\/p>\n<p>Sheath folds related to Late Miocene shearing in the Calanchiole Marble, within the Calamita Unit. This is a N-S oriented outcrop, perpendicular to the E-W trending lineation and shows ellipse-like sections through these strongly non-cylindrical folds.<\/p>\n<p>The field of view is approximately 2 – 3 m.<\/p>\n<p><strong>Photo credits:<\/strong>\u00a0Samuele Papeschi<\/p>\n<p><strong>References:<br \/>\n<\/strong>Papeschi, S., Musumeci, G., & Mazzarini, F. (2017). Heterogeneous brittle-ductile deformation at shallow crustal levels under high thermal conditions: The case of a synkinematic contact aureole in the inner northern Apennines, southeastern Elba Island, Italy.\u00a0<i>Tectonophysics<\/i>,\u00a0<i>717<\/i>, 547-564. <a href=\"https:\/\/doi.org\/10.1016\/j.tecto.2017.08.020\">https:\/\/doi.org\/10.1016\/j.tecto.2017.08.020<\/a><\/p>\n","modified":"2020-07-27T16:42:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0189-1024x768.jpg","taxonomy":{"webmapp_category":[229,232,234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7598","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7598&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/sheath-folds-in-mylonitic-marble\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.407424472613,42.715183227086]}},{"type":"Feature","properties":{"id":7590,"name":"Folds on Fm. Trubi (Southern Sicily)","description":"","modified":"2020-07-25T17:33:08","color":"","icon":"","noDetails":false,"noInteraction":false,"imageGallery":[{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_20200722_160131_BURST1-472x1024.jpg","id":7591,"caption":""}],"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_20200722_160131_BURST1-472x1024.jpg","taxonomy":{"webmapp_category":[229,235]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7590","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7590&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/folds-on-fm-trubi-southern-sicily-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[13.726478551573,37.170449743776]}},{"type":"Feature","properties":{"id":7577,"name":"Glaucophane-bearing metabasite in mylonitic calcschists","description":"<p><img loading=\"lazy\" class=\"alignnone size-full wp-image-7578\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-scaled.jpg\" alt=\"\" width=\"2560\" height=\"1920\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-scaled.jpg 2560w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-1536x1152.jpg 1536w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-2048x1536.jpg 2048w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-1080x810.jpg 1080w\" sizes=\"(max-width: 2560px) 100vw, 2560px\" \/>Lenses of boundinated green metabasite (containing relic glaucophane, lawsonite, omphacite) surrounded by glaucophane-albite-epidote-bearing mylonitic calcschist and marble.<\/p>\n<p>Peak P-T conditions in these rocks were estimated to be around 1.5 – 1.8 GPa and 300 – 400 \u00b0C.<\/p>\n<p>The field of view is approximately 5 – 7 m.<\/p>\n<p><strong>Photo credits:<\/strong>\u00a0Samuele Papeschi<\/p>\n<p><strong>References:<br \/>\n<\/strong>Papeschi, S., Musumeci, G., Massonne, H. J., Mazzarini, F., Ryan, E. J., & Viola, G. (2020). High\u2010P (P= 1.5\u20131.8 GPa) blueschist from Elba: Implications for underthrusting and exhumation of continental units in the Northern Apennines.\u00a0<i>Journal of Metamorphic Geology<\/i>, 38, 495-525.<br \/>\n<a href=\"https:\/\/doi.org\/10.1029\/2019TC005890\">https:\/\/doi.org\/10.1029\/2019TC005890<\/a><strong><br \/>\n<\/strong><\/p>\n","modified":"2020-07-13T16:26:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0416-1024x768.jpg","taxonomy":{"webmapp_category":[228,232,234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7577","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7577&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/glaucophane-bearing-metabasite-in-mylonitic-calcschists\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.431552464307,42.81525425844]}},{"type":"Feature","properties":{"id":7572,"name":"Leucocratic dykes cutting across migmatitic schists","description":"<p><img loading=\"lazy\" class=\"size-full wp-image-7573\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-scaled.jpg\" alt=\"\" width=\"2560\" height=\"1920\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-scaled.jpg 2560w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-1536x1152.jpg 1536w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-2048x1536.jpg 2048w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-1080x810.jpg 1080w\" sizes=\"(max-width: 2560px) 100vw, 2560px\" \/><\/p>\n<p>Leucogranite dykes (K-feldspar + quartz + tourmaline \u00b1 white mica) cross cutting E-dipping schist and quartzite with migmatitic structures (paragenesis: biotite + andalusite + cordierite + K-feldspar + plagioclase + quartz).<\/p>\n<p><strong>Photo credits:<\/strong> Samuele Papeschi<\/p>\n<p><strong>References:<br \/>\n<\/strong>Papeschi, S., Musumeci, G., Massonne, H.J., Bartoli, O., & Cesare, B. (2019). Partial melting and strain localization in metapelites at very low-pressure conditions: The northern Apennines magmatic arc on the Island of Elba, Italy. <em>Lithos,<\/em> 350, 105230. <a href=\"https:\/\/doi.org\/10.1016\/j.lithos.2019.105230\">https:\/\/doi.org\/10.1016\/j.lithos.2019.105230<\/a><\/p>\n","modified":"2020-07-13T16:26:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/07\/IMG_0097-1024x768.jpg","taxonomy":{"webmapp_category":[232,224,234,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7572","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7572&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/leucocratic-dykes-cutting-across-migmatitic-schists\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.434377500952,42.725311800884]}},{"type":"Feature","properties":{"id":7514,"name":"S-C mylonites in the Calamita Schists","description":"<p><img loading=\"lazy\" class=\"wp-image-7515 aligncenter\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-300x225.jpg\" alt=\"\" width=\"793\" height=\"595\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1536x1152.jpg 1536w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-2048x1536.jpg 2048w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1080x810.jpg 1080w\" sizes=\"(max-width: 793px) 100vw, 793px\" \/><br \/>\nS-C mylonites developed in andalusite-cordierite micaschist (Calamita Schists) in the contact aureole of the Porto Azzurro pluton. The white layers are made of quartz, while the brown layers consist predominantly of white mica and biotite. Top-to-left (East) sense of shear.<\/p>\n<p><strong>Photo credits:<\/strong> Samuele Papeschi<\/p>\n<p><strong>References:<\/strong><br \/>\nPapeschi, S., Musumeci, G., & Mazzarini, F. (2017). Heterogeneous brittle-ductile deformation at shallow crustal levels under high thermal conditions: The case of a synkinematic contact aureole in the inner northern Apennines, southeastern Elba Island, Italy.\u00a0<i>Tectonophysics<\/i>,\u00a0<i>717<\/i>, 547-564. https:\/\/doi.org\/10.1016\/j.tecto.2017.08.020<\/p>\n<p>Papeschi, S., Musumeci, G., & Mazzarini, F. (2018). Evolution of shear zones through the brittle-ductile transition: The Calamita Schists (Elba Island, Italy).\u00a0<i>Journal of Structural Geology<\/i>,\u00a0<i>113<\/i>, 100-114. https:\/\/doi.org\/10.1016\/j.jsg.2018.05.023<\/p>\n","modified":"2020-07-04T14:40:47","color":"","icon":"","noDetails":false,"noInteraction":false,"imageGallery":[{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1024x768.jpg","id":7515,"caption":""}],"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/IMG_0010-1024x768.jpg","taxonomy":{"webmapp_category":[234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7514","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7514&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/s-c-mylonites-in-the-calamita-schists\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.382609525860213,42.71506838353767]}},{"type":"Feature","properties":{"id":7491,"name":"Mylonitic schists of the Ferriere-Molli\u00e8res shear zone","description":"<p>Here we can observe the most classic mylonites of the Ferriere-Molli\u00e8res shear zone. Medium grained dark-green mylonitic schist (fig. 4a) made up of quartz, K-feldspar and plagioclase porphyroclasts in a fine grained biotite and white mica matrix (fig. 4b). Sometimes garnet porphyroclasts are present. The amount of matrix is nearly 75%. Both at the meso and micro scale kinematic indicators are well recognizable. They are mainly represented by rotated porphyroclasts, S-C\u2019 fabric, micafish and quartz oblique foliation representing a top-to-the SE sense of shear.<\/p>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div><\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/div>\n<\/div>\n<div><\/div>\n","modified":"2021-02-08T21:58:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/Fig.-4-1024x383.jpg","accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7491","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7491&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mylonitic-schists-of-the-ferriere-mollieres-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.994944,44.312272]}},{"type":"Feature","properties":{"id":7489,"name":"Protomylonites of the Ferriere-Molli\u00e8res shear zone","description":"<p>Coarse grained protomylonitic gneiss (fig. 2a) with deformed leucosomes of K-feldspar, plagioclase and quartz in a medium grained biotite and sillimanite matrix with sometimes white mica. The amount of matrix is variable from a maximum of nearly 50% to a minimum of 30% – 40%. S-C fabric and asimmetric and stretched leucosomes are recognizable (fig. 2a), All the kinematic indicators point to a top-to-the SE sense of shear (fig. 2b).<\/p>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/p>\n<\/div>\n<\/div>\n<div><\/div>\n<div id=\"finestramailtomailModalToPopup\" style=\"z-index: 1102;\">\n<div id=\"finestramailtomailContentPopup\">\n<div id=\"finestramailtotoClose\"><\/div>\n<div id=\"finestramailtotoModalPopup\">What do you want to do ?<\/div>\n<p><a id=\"finestramailtonewButtonEmail\"><\/a>New mail<button id=\"finestramailtocopyClipboardEmail\">Copy<\/button><textarea id=\"finestramailtotoTextCopyAreaSelect\"><\/textarea><\/div>\n<\/div>\n<div><img \/><\/div>\n","modified":"2021-02-08T21:55:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2020\/06\/Fig.-2-1024x382.jpg","accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7489","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7489&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/protomylonites-of-the-ferriere-mollieres-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.976554,44.310514]}},{"type":"Feature","properties":{"id":7447,"name":"Cross-bedding sandstones in Marseille basin","description":"<p>The clast size is variable from fine sand\/silt to gravel.<br \/>\nPicture by Anne-Sabine Grosjean and Baptiste 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Photo by Chiara Montomoli<\/p>\n","modified":"2019-10-06T20:27:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/DSCN8672-1024x768.jpg","taxonomy":{"webmapp_category":[228]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7216","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7216&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/boudinage-in-quarzitic-levels-interbedded-with-phillites-northern-apennines-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.527336660745732,43.79872651155583]}},{"type":"Feature","properties":{"id":7200,"name":"Lochsite","description":"<p>The Glarus Thrust: In Switzerland\u2019s most famous geological outcrop at the Lochsite, 250-300 million-year-old Verrucano rocks rest on younger, 35-50 million-year-old Flysch rocks. Since the 19th century, fundamental insights into the formation of the Alps have been gained here. Specifically, scientists understood the way mountains form as a result of overthrusts. Previously, earth scientists had assumed that mountains were formed due to the shrinkage of the earth in connection with the mantle cooling.<\/p>\n<p>After visiting the Lochsite, it is clear to everyone that \u201calpine folding\u201d never happened!<\/p>\n<p> <\/p>\n","modified":"2020-05-09T10:15:24","color":"","icon":"","noDetails":false,"noInteraction":false,"imageGallery":[{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/Lochsite_Detail-1-1024x926.jpg","id":7441,"caption":""},{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/Schils_Lochsite-1-1024x682.jpg","id":7440,"caption":""},{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/Inszenierung_Lochsite.jpg","id":7208,"caption":"Photo by: Tektonikarena Sardona"},{"src":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/Strukturen_Lochsite_3D_Buckingham-1024x724.jpg","id":7205,"caption":"Photo by: Thomas Buckingham"}],"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/10\/Schils_Lochsite-1-1024x682.jpg","taxonomy":{"webmapp_category":[220,224,230,231]},"accessibility":{"mobility":{"check":true,"description":"<p><strong>Access by public transport<\/strong>: Train to <strong>“Glarus S\u00fcd”<\/strong> and after bus to <strong>“Wart”<\/strong> <span class=\"desktop-title-subcontent\">(8762 Glarus S\u00fcd)<\/span><\/p>\n<p>Public transport Switzerland <a href=\"https:\/\/www.sbb.ch\/en\/home.html\">https:\/\/www.sbb.ch\/en\/home.html<\/a><\/p>\n<p><strong>Access by car<\/strong> from Glarus S\u00fcd: follow Sernftalstrasse in direction ELm, after 6 minutes you will see the installation of “Lochsite” and a parking lot<\/p>\n"},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"related_url":["https:\/\/unesco-sardona.ch\/erlebnis\/lochsite"],"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7200","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7200&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/lochsite-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"+41 81 723 59 20","contact:email":"info@unesco-sardona.ch","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.091614036983856,46.997288304920126]}},{"type":"Feature","properties":{"id":7186,"name":"Fold in the Helvetic Wildhorn nappe","description":"<p>Rverese folds close to Sanetsch dam (Switzerland):\u00a0 the frontal part of the Helvetic Wildhorn nappe. Note the occurrence of normal faults in the normal limb of the fold (Urgonian limestone).<\/p>\n<p>Photo by R. Carosi – HKT workshop, pre conference field trip, Lausanne 2018<\/p>\n","modified":"2019-10-01T18:32:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/09\/IMG_1124-1024x768.jpeg","accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7186","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7186&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/fold-in-the-helvetic-wildhorn-nappe\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.302128107470708,46.36992395759198]}},{"type":"Feature","properties":{"id":7161,"name":"Coriscao syncline","description":"<p>The eastern face of the Coriscao peak (2235m) in the Cantabrian Mountains, (NW Spain) shows the deformation associated with the external nappes of the Cantabrian Zone (NW Iberian Massif) during the Variscan Orogeny. The Panda Fm. limestones (Moscovian) were thrust on top of the Coriscao Fm. olistrostrome (Moscovian), and subsequently folded by the Coriscao syncline.<\/p>\n","modified":"2019-09-26T11:22:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/09\/3_El-sinclinal-nevado-del-Coriscao2-1024x681.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7161","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7161&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/coriscao-syncline\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.778738389639102,43.090446431918664]}},{"type":"Feature","properties":{"id":7148,"name":"Magmatic foliation in a granodiorite, Elba island Italy","description":"<p>Magmatic foliation in the Monte Capanne granodiorite, S. Andrea locality, Elba island Italy<\/p>\n<p>The foliation is highlighted by cm-scale k-feldspar. Two rounded mafic enclaves occurrs on the right.<\/p>\n","modified":"2019-08-29T10:15:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/08\/IMG_4281-225x300.jpg","taxonomy":{"webmapp_category":[232,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7148","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7148&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/magmatic-foliation-in-a-granodiorite-elba-island-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.14093058483354,42.808671301450886]}},{"type":"Feature","properties":{"id":7128,"name":"Antiform, Pania di Corfino (Northern Apennines)","description":"<p>Panoramic view of the kilometric large-scale F2\u00a0 fold (open antiform) in the Corfino area involving the Tuscan Nappe (Calcare massiccio\u201d formation on top and \u201cCalcari & Marne a Rhaetavicula contorta\u201d formation below with eviedence of bedding). Mount La Bandita view to the west.<\/p>\n<p>Ref. Carosi et al 2004 Geodinamica Acta 17 (2004) 253\u2013273<\/p>\n","modified":"2019-08-29T10:18:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/IMG_4503-300x225.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7128","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7128&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/antiform-pania-di-corfino-northern-apennines\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.408263900061002,44.18231481013327]}},{"type":"Feature","properties":{"id":7122,"name":"S-C fabric, normal fault, Sasso Rosso (N Apennines)","description":"<p>S-C fabric along a normal fautl in Jurassic limestone. Sasso Rosso, Northern Apennines<\/p>\n","modified":"2019-08-29T10:14:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/IMG_4513-1-265x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7122","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7122&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/s-c-fabric-normal-fault-sasso-rosso-n-apennines\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.40031383254086,44.18356121276769]}},{"type":"Feature","properties":{"id":7097,"name":"Badlands on Pliocene limestone (Fm. Monte Narbone, Southern Sicily)","description":"<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-7098\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/20190708_1845561-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/20190708_1845561-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/20190708_1845561-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/20190708_1845561-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/20190708_1845561-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/20190708_1845561-1080x810.jpg 1080w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/p>\n","modified":"2019-07-13T10:03:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/07\/20190708_1845521-1024x768.jpg","taxonomy":{"webmapp_category":[235,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7097","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7097&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/badlands-on-pliocene-limestone-fm-monte-narbone-southern-sicily\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[13.682421518504611,37.1891975392557]}},{"type":"Feature","properties":{"id":7061,"name":"Seismites","description":"<p>Soft sediment deformation in the Lisan Formation of the Lacustrine sediments – Nahal Prazim Dead Sea.\u00a0 Israel.\u00a0 The deformation folding is due to an earthquake followed by a tsunami in the Lake Lisan, a precursor lake to the Dead Sea.<\/p>\n","modified":"2019-06-21T11:23:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P8069935-1024x768.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7061","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7061&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/seismites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[35.36199552139908,31.08237556437035]}},{"type":"Feature","properties":{"id":7054,"name":"Intense ductile deformation","description":"<p>Ex feldspar crystals developed in mantled \u03b4-type porphyroclasts affecting mylonitic texture orthogneiss (“augengneiss”).\u00a0 Dextral sense of shear (top-to-right ductile shear zone).\u00a0 Outcrop photo originally vertical, from the Engadine valley (outcrops probably associated to Engadine Line), near St. Moritz (20km south of St.Moritz towards Como lake), Rhetic Alps, central Alps, Switzerland.<\/p>\n","modified":"2019-06-21T11:20:24","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/46-1024x734.jpg","taxonomy":{"webmapp_category":[234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7054","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7054&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/intense-ductile-deformation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.69975255446218,46.39600241775577]}},{"type":"Feature","properties":{"id":7043,"name":"Oblique stratification in Upper Jurassic limestones","description":"<p><img loading=\"lazy\" class=\"alignnone size-large wp-image-7044\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110017-1024x768.jpg\" alt=\"\" width=\"1024\" height=\"768\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110017-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110017-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110017-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110017-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110017-1080x810.jpg 1080w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/p>\n<p>Oblique stratification in Tithonian limestones at Huveaune source in Sainte-Baume near Aubagne, France. The age is uncertain, it is refered as “Portlandian” in the geological map (Cuers 1\/50 000 n\u00b01045).<\/p>\n<p>Picture by Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-06-16T21:45:48","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110017-1024x768.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7043","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7043&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/oblique-stratification-in-upper-jurassic-limestones\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.762228,43.345873]}},{"type":"Feature","properties":{"id":7040,"name":"Travertine of the Huveaune source, France","description":"<p><img loading=\"lazy\" class=\"alignnone size-large wp-image-7041\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-1024x768.jpg\" alt=\"\" width=\"1024\" height=\"768\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-1080x810.jpg 1080w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/p>\n<p>Modern travertine of the Huveaune source in Sainte-Baume near Aubagne, France.<\/p>\n<p>Picture By Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-06-16T21:44:59","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5110009-1024x768.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7040","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7040&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/travertine-of-the-huveaune-source-france\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.764099,43.348645]}},{"type":"Feature","properties":{"id":7032,"name":"Carboniferous\/Triassic discontinuity at clues de Verdaches, France","description":"<p><img loading=\"lazy\" class=\"alignnone size-large wp-image-7033\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P6100120-1024x768.jpg\" alt=\"\" width=\"1024\" height=\"768\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P6100120-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P6100120-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P6100120-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P6100120-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P6100120-1080x810.jpg 1080w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/>The carboniferous is composed of channelized fine sandstones in silty floodplain. Some levels are very rich in organic matter and some plants can be found such as ferns. The Triassic is composed of channelized quartzite with beautiful lateral accretions. The contact forms a nice angular discontinuity.<\/p>\n<p>Picture by Anne-Sabine Grosjean and Baptiste Such\u00e9ras-Marx<\/p>\n","modified":"2019-06-16T21:44:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P6100120-1024x768.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7032","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7032&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/carboniferous-triassic-discontinuity-at-clues-de-verdaches-france\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.299875974655151,44.273380127975365]}},{"type":"Feature","properties":{"id":7029,"name":"Fault and fold in calcschist of Giens near Hy\u00e8res, France","description":"<p><img loading=\"lazy\" class=\"alignnone size-large wp-image-7030\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5300027-e1560706656114-768x1024.jpg\" alt=\"\" width=\"768\" height=\"1024\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5300027-e1560706656114-768x1024.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5300027-e1560706656114-225x300.jpg 225w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5300027-e1560706656114-1080x1440.jpg 1080w\" sizes=\"(max-width: 768px) 100vw, 768px\" \/><\/p>\n<p>Giens peninsula (near Hy\u00e8res, France) has beautiful outcrops of metamorphic rocks. Some are folded and faulted like on this picture on the western side of the peninsula.<\/p>\n","modified":"2019-06-16T19:45:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/P5300027-e1560706656114-768x1024.jpg","taxonomy":{"webmapp_category":[220,229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7029","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7029&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/fault-and-fold-in-calcschist-of-giens-near-hyeres-france\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.096309,43.028767]}},{"type":"Feature","properties":{"id":7015,"name":"thrusts intra-nappe double up australpine mesozoic cover (Ortles nappe) Rhetic Alps","description":"<h4><span style=\"color: #ccffcc;\">Corne del Palone mount\u00a0thrusts intra-nappe thrusts double up australpine mesozoic cover (Ortles nappe) made of “Fraele formation” + “Dolomia del Cristallo formation” (Triassic), just under regional importance thrust (Alpisella Line), at the top of Corne del Palone mount, where Ortles nappe is <em>overthrusted by<\/em>\u00a0“Dolomia dello Stelvio” belonging to Quattervals nappe, australpine domain. Southern slopes of\u00a0Corne del Palone mount, towards <\/span><span style=\"color: #ccffcc;\">Stelvio Pass,Braulio Valley, high eastern Valtellina,\u00a0<em>Rhetic Alps, Lombardy.<\/em><\/span><\/h4>\n<h4><em><img loading=\"lazy\" class=\"alignnone size-medium wp-image-7016\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-510x382.jpg 510w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><img loading=\"lazy\" class=\"alignnone size-medium wp-image-7017\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-2-300x184.jpg\" alt=\"\" width=\"300\" height=\"184\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-2-300x184.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-2-768x472.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-2.jpg 902w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/em><\/h4>\n<h4><span style=\"color: #ccffcc;\">(Photo by Lorusso Angelo)<\/span><\/h4>\n","modified":"2019-06-15T13:19:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Corne-del-Palone-vs-P.Stelvio-Valle-Braulio-thrust-raddop-cop-falda-Ortles-australp-inf-sotto-Linea-Alpisella-1024x768.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7015","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7015&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/thrusts-intra-nappe-double-up-australpine-mesozoic-cover-ortles-nappe-rhetic-alps\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.368900560383395,46.51367560697147]}},{"type":"Feature","properties":{"id":7005,"name":"syntectonic granite sheets","description":"<div id=\"attachment_7002\" style=\"width: 310px\" class=\"wp-caption alignnone\"><img aria-describedby=\"caption-attachment-7002\" loading=\"lazy\" class=\"size-medium wp-image-7002\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00425-1080x810.jpg 1080w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-7002\" class=\"wp-caption-text\">Syntectonic granite sheets Salknappen, Antarctica.<\/p><\/div>\n<div id=\"attachment_7006\" style=\"width: 310px\" class=\"wp-caption alignnone\"><img aria-describedby=\"caption-attachment-7006\" loading=\"lazy\" class=\"size-medium wp-image-7006\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/DSC00426-1080x810.jpg 1080w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-7006\" class=\"wp-caption-text\">Syntectonic granite sheets at Salknappen, Antarctica<\/p><\/div>\n<p>Steeply dipping discordant pegmatite veins are crosscut by layering parallel granite sheets along which extensional top to South syntectonic displacement has occurred at ~490Ma. Person at bottom for scale. Extensional shears parallel to the pegmatite veins are evident.<\/p>\n","modified":"2019-06-07T22:53:34","color":"","icon":"","noDetails":false,"noInteraction":false,"taxonomy":{"webmapp_category":[224,219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/7005","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=7005&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/syntectonic-granite-sheets\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.00582449859985,-72.323492195148]}},{"type":"Feature","properties":{"id":6988,"name":"Messinian Gypsum outcrop in Southern Sicily","description":"<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-6989\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Inked20190602_103302_LI-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Inked20190602_103302_LI-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Inked20190602_103302_LI-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Inked20190602_103302_LI-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Inked20190602_103302_LI-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/Inked20190602_103302_LI-1080x810.jpg 1080w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/> <img loading=\"lazy\" class=\"alignnone size-medium wp-image-6990\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/20190602_103219-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/20190602_103219-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/20190602_103219-768x576.jpg 768w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/20190602_103219-1024x768.jpg 1024w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/20190602_103219-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/20190602_103219-1080x810.jpg 1080w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/p>\n","modified":"2019-06-07T16:40:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/06\/20190602_103219-1024x768.jpg","taxonomy":{"webmapp_category":[235,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6988","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6988&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/messinian-gypsum-outcrop-in-southern-sicily\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[13.757673136977814,37.19098389762568]}},{"type":"Feature","properties":{"id":6978,"name":"Folded Flysch Farini d’Olmo (Paleocene -Eocene) – Piacenza (Italy)","description":"<p>Folded Flysch Farini d’Olmo (Paleocene -Eocene) – Piacenza (Italy)<\/p>\n","modified":"2019-05-29T19:00:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/2017-07-30-Flysch-Farini-commentata-1024x686.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6978","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6978&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/folded-flysch-farini-dolmo-paleocene-eocene-piacenza-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.580061743200645,44.72260212911179]}},{"type":"Feature","properties":{"id":6970,"name":"Interference of F1 and F2 folds, Orto di Donna, Lucca, Italy","description":"<p>Tyoe 3 interference pattern of folds in Selcifero limestone, Orto di Donna, Lucca, Italy.<\/p>\n<p>Layers of Selcifero limestone and F1 steeply diping axial planes are refolded by F2 folds with shallowly dipping axial planes giving rise to type 3 interference pattern (Ramsay, 1967). A F1 fold hinge is observable close to the center of the photo highlighted by withish cherts layers with M secondary folds.<\/p>\n","modified":"2019-06-07T16:45:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/Orto-di-Donna-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6970","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6970&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/interference-of-f1-and-f2-folds-orto-di-donna-lucca-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.19580936438524,44.13535574040764]}},{"type":"Feature","properties":{"id":6952,"name":"Cumulites, Mattarana, Italy","description":"<p>Olivine adcumulus within the gabbro massif, Internal Liguride Units, Mattarana quarry, La Spezia Italy.<\/p>\n","modified":"2019-06-07T16:46:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/Cumuliti-mattarana-300x225.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6952","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6952&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/cumulites-mattarana-italy\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.585013689981452,44.24688451846203]}},{"type":"Feature","properties":{"id":6957,"name":"Ophicalcite, Montaretto, La Spezia","description":"<p>Block of ophicalcite in the quarry of Monteretto, La Spezia, Italy.<\/p>\n<p>The typical brittle deformation of mantle ophicalcite.<\/p>\n<p> <\/p>\n<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-6966\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/breccia-levanto-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/breccia-levanto-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/breccia-levanto-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/breccia-levanto.jpg 640w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/p>\n<p> <\/p>\n<p><img loading=\"lazy\" class=\"alignnone size-medium wp-image-6961\" src=\"http:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/breccia-levanto-Montaretto-300x225.jpg\" alt=\"\" width=\"300\" height=\"225\" srcset=\"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/breccia-levanto-Montaretto-300x225.jpg 300w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/breccia-levanto-Montaretto-510x382.jpg 510w, https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/breccia-levanto-Montaretto.jpg 640w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/p>\n","modified":"2019-06-07T16:46:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/blocco-levanto-Montaretto-300x225.jpg","taxonomy":{"webmapp_category":[220,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6957","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6957&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/ophicalcite-montaretto-la-spezia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.58892429176285,44.19776670828329]}},{"type":"Feature","properties":{"id":6947,"name":"Sigma-type clinopyroxene porphyroclast in HT shear zone","description":"<p>Sigma-type clinopyroxene porphyroclast (top to the left) in High Temperature shear zone in gabbros, Internal Ligurian Units, Bonassola, Italy<\/p>\n<p>Photo by Rodolfo Carosi (Unito)<\/p>\n","modified":"2019-06-07T16:47:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/05\/HT-shear-zone-Bonassola-1024x720.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6947","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6947&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/sigma-type-clinopyroxene-porphyroclast-in-ht-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.584211162992915,44.18012474020711]}},{"type":"Feature","properties":{"id":6933,"name":"Folds and metasomatized, retrogressed ex garnet peridotite (now serpentinized) boudins within amphibole-bearing migmatitic gneiss, Borgo outcrop Darengo Valley, Adula nappe","description":"<p>Interference patterns in metric refolded folds described by layering foliation traces in Adula nappe crystalline basement with , Borgo outcrop at the confluence Darengo – Led\u00f9 streams, southern steep zone of Adula nappe (ex) “roots zone” (Southern Steep Belt), Adula nappe ancient southern paleoeuropean continental margin, Penninic domain, Darengo Valley, “Costiera dei Muncech”, Mesolcina Range, Eastern Lepontin<span style=\"line-height: 1.7em;\">e Alps. Central Alps, Lombardy region, northern Italy.<\/span><\/p>\n<p>(Photo by Lorusso Angelo)<\/p>\n<p> 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Gemignani, L. Godin, Iaccarino S., Larson K. P., Montomoli C., Rai S. M. (2014) – A geological journey in the deepest canyon of the earth: the Kali Gandaki section Rodolfo. . In: (Eds.) Chiara Montomoli, Rodolfo Carosi, Rick Law, Sandeep Singh, and Santa Man Rai, Journal of the Virtual Explorer, volume 47, paper 9, 1-31.<\/p>\n","modified":"2019-02-04T21:21:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2019\/02\/Larjung-composizione-foto-1024x686.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6533","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6533&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/folds-in-the-annapurna-yellow-formation-kaligandaki-nepal\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.59598293989393,28.67216703851193]}},{"type":"Feature","properties":{"id":6516,"name":"Sapphirine bearing granulites from Gruf Compex, Penninic Domain, index of U.H.T. – “Ultra High Temperature” metamorphism in central (italian Rethic) Alps","description":"<p>Sapphirine bearing granulites from Gruf Compex, Penninic Domain, index of U.H.T. – “Ultra High Temperature” metamorphism in central (italian Rethic) Alps.These granulites (type A of Galli et al. 2011) are rare, dark, heavy and massive rocks normally occurred as relict enclaves in migmatitic orthogneisses and charnockites and represent restitic melanocratic refractory product as residue compliments originating through melt extraction from prepermian metapelitic sediments showi<span class=\"text_exposed_show\">ng mineral assemblage made of orthopyroxene (honey light-brown), sapphirine (blue), biotite (dark brown), garnet (pink with opx\u2013cordierite symplectites inside), quartz (colourless), feldspar (grey). 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Donegal, Ireland","description":"","modified":"2018-12-14T11:09:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Fold-8JPG-768x1024.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6083","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6083&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/cashelgolan-co-donegal-ireland\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-8.397561575920463,54.84407671782797]}},{"type":"Feature","properties":{"id":6025,"name":"Cashelgolan, Co. 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Donegal, Ireland","description":"<p>Near Slieve League, highest sea-cliffs in west Europe.<\/p>\n","modified":"2018-12-14T11:08:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Bunglass-Point-1024x768.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6094","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6094&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/bunglass-point-carrick-co-donegal-ireland\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-8.686220171948662,54.62705267588337]}},{"type":"Feature","properties":{"id":6086,"name":"St John’s Point, Co. Donegal , Ireland","description":"","modified":"2018-12-14T11:07:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/St-Johns-Point-1024x765.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6086","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6086&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/st-johns-point-co-donegal-ireland\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-8.451647994367022,54.57745957141567]}},{"type":"Feature","properties":{"id":6064,"name":"Thrust sheets in Via del\u2019Amore","description":"<p>Mesoscale thrust sheets within the Tuscan nappe of the Apenninic fold-and-thrust belt.<\/p>\n<p>Photo by Adriana G. Fl\u00f3rez<\/p>\n","modified":"2018-12-12T15:28:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Thrust-sheets-01-1024x676.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6064","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6064&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/thrust-sheets-in-via-delamore-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.73425112013615,44.100118437748634]}},{"type":"Feature","properties":{"id":6073,"name":"Domino-boudin","description":"<p>Domino-boudin in the Complejo Metam\u00f3rfico de Bah\u00eda Mansa, Chile (paleo-accretionary prism context). Photo Gaelle Plissart<\/p>\n","modified":"2018-12-12T15:05:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/DSC07227-1024x768.jpg","taxonomy":{"webmapp_category":[228]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6073","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6073&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/domino-boudin-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-73.84568282870748,-40.912991853748544]}},{"type":"Feature","properties":{"id":5979,"name":"Folded gabbro dyke in serpentinites","description":"<p>Folded gabbro dyke in serpentinites with subvertical axial plane, parallel to the main foliation. Lanzo Massif.<br \/>\nBalme, Pian della Mussa<\/p>\n","modified":"2018-12-21T14:16:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/DSC_2487-1024x678.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5979","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5979&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/folded-gabbro-dyke-in-serpentinites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.221077156429942,45.30340974533686]}},{"type":"Feature","properties":{"id":5967,"name":"Kinked schist, Malfatano beach","description":"<p>Kinked folds in the Bithia Schists (Cambrian) (Malfatano beach, southern Sardinia).<\/p>\n","modified":"2018-12-21T14:19:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/DSC_0490-1024x678.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5967","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5967&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/kinked-schist-malfatano-beach\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.800785620799502,38.89166278326032]}},{"type":"Feature","properties":{"id":5985,"name":"A meso-scale faulted multi-detachment fold, Khabr area, Kerman, Iran","description":"<p>Fault-related folding is an important process in compressive belts (Mukherjee et al. 2015). This horizontal section photograph shows a textbook example of a detachment horizon, which has developed asymmetric detachment fold (\u201cA\u201d in Fig. 1), fault-propagation fold (\u201cB\u201d in Fig. 1), and a box-fold (\u201cC\u201d in Fig. 1). The structure in the middl<span class=\"text_exposed_show\">e of the photo (\u201cB\u201d in Fig. 1) is plausibly a fold-propagation fold, where white thin beds of laminated marble is sitting as an intermediate detachment horizon (Fig. 1). The fold geometry (\u201cB\u201d in Fig. 1) is usually tighter structure than asymmetric detachment fold with a long, gently dipping backlimb and a shorter, steeply dipping forelimb. The larger fold structure in the right side (\u201cC\u201d in Fig. 1) is more complex, with multiple sharp hinges separating straight limbs as a box lift-off anticline (e.g. McClay 1992; Mitra 2002, 2003) and small scale offsets due to penetrative strain (Burberry 2015). This fold is tighter in the core. See Mukherjee (2012) for a similar kind of fold in micro-scale.<br \/>\nThese structures are well developed within the sequence of Devonian alternating layers of calcschist, meta-limestone turbidite (brown) and thin bands of laminated marble (white) and affected by east trending dextral Khabr shear zone with moderate dip to the north. This photo is taken from the Khabr Mountain (height: 3845m) (Geographic coordinates: 28\u00b052\u00b404\u02baN, 56\u00b023\u00b456\u02baE), Structural zone of Sanandaj-Sirjan metamorphic-ophiolitic Complex, southwest of the city of Baft, Kerman province, Iran.<\/span><\/p>\n<p>A meso-scale faulted multi-detachment fold, Khabr area, Kerman, Iran, Photo by Seyed Tohid Nabavi<\/p>\n","modified":"2018-12-12T15:07:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/Picture1-1-1024x579.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5985","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5985&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/a-meso-scale-faulted-multi-detachment-fold-khabr-area-kerman-iran\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[56.43751508107118,28.802959234513224]}},{"type":"Feature","properties":{"id":6045,"name":"Nonconformity","description":"<p>Devonian Horton Group sandstone\u00a0nonconformably\u00a0overlying gneiss in Timber Brook. Equivalent to Hutton’s unconformity in Scotland.<\/p>\n","modified":"2018-12-12T12:56:59","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/timberbrook-300x194.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6045","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6045&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/nonconformity\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-60.659207932695324,46.3250513049117]}},{"type":"Feature","properties":{"id":6016,"name":"Cilindro de Marbor\u00e9","description":"<p>Monte Perdido, in the Central Pyrenees, constitutes the highest limestone massif in Europe, rising to the maximum height of 3355 m.a.s.l. of Monte Perdido peak. Looking west from the summit a spectacular anticlinal fold can be observed below the nearby Cilindro de Marbor\u00e9 peak (3328 m.a.s.l.). The fold is developed in a stacked Cretaceous-Paleogene sequence (Marbor\u00e9, Salarons and Gallinera Formations) deformed by thin-skinned tectonics in the imbricated thrust system of Monte Perdido unit. Later emplacement of the major Gavarnie basement thrust was accompanied by refolding of the Meso-Cenozoic sedimentary cover of its hangingwall (Flach\u00e8re, 1977. Th\u00e8se 3 cycle, Toulouse), of which this anticlinal is an extraordinary example. A paired syncline, mostly covered by scree, is located left of the main structure. The height difference between the Cilindro de Marbor\u00e9 summit and the Ib\u00f3n Helado, the lake just below it is of 350m.<\/p>\n<p>de Paz-\u00c1lvarez, M.I., Fl\u00f3rez-Rodr\u00edguez, A.G. (2018). Photograph of the month. <em>Journal of Structural Geology<\/em>, 111, iii.<\/p>\n<p> <\/p>\n","modified":"2018-12-12T10:05:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/12\/23613466591_5e44b769b5_k-1-1024x555.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/6016","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=6016&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/cilindro-de-marbore\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[0.032573312104659635,42.67723635993417]}},{"type":"Feature","properties":{"id":5745,"name":"Kyanite","description":"<p>Kyanite bearing micaschist, Bruncu Nieddu.<\/p>\n<p><span class=\"Apple-style-span\"><span class=\"SpellE\">About<\/span> 0.5 km <span class=\"SpellE\">further<\/span> <span class=\"SpellE\">north<\/span> <span class=\"SpellE\">along<\/span> the <span class=\"SpellE\">track<\/span> <span class=\"SpellE\">we<\/span> <span class=\"SpellE\">reach<\/span> the <span class=\"SpellE\">kyanite+biotite<\/span> <span class=\"SpellE\">isograd<\/span> <span class=\"SpellE\">with<\/span>mm- <span class=\"SpellE\">to<\/span> <span class=\"SpellE\">cm-size<\/span> <span class=\"SpellE\">bluish<\/span> <span class=\"SpellE\">kyanite<\/span> <span class=\"SpellE\">crystals<\/span> in the <span class=\"SpellE\">matrix<\/span> <span class=\"SpellE\">of<\/span> the <span class=\"SpellE\">mylonites<\/span> and in <span class=\"SpellE\">quartz-rich<\/span> <span class=\"SpellE\">veins<\/span> (Fig. 1). The <span class=\"SpellE\">kyanite+biotite<\/span> <span class=\"SpellE\">isograd<\/span> <span class=\"SpellE\">is<\/span> <span class=\"SpellE\">marked<\/span> <span class=\"SpellE\">by<\/span> the first <span class=\"SpellE\">appearance<\/span> <span class=\"SpellE\">of<\/span><span class=\"SpellE\">kyanite<\/span> <span class=\"SpellE\">crystals<\/span>. The <span class=\"SpellE\">rocks<\/span> <span class=\"SpellE\">consist<\/span> <span class=\"SpellE\">of<\/span> <span class=\"SpellE\">porphyroblasts<\/span> <span class=\"SpellE\">of<\/span> staurolite, <span class=\"SpellE\">kyanite<\/span>, and<span class=\"SpellE\">plagioclase<\/span> <span class=\"SpellE\">enveloped<\/span> in a <span class=\"SpellE\">mylonitic<\/span> <span class=\"SpellE\">matrix<\/span> <span class=\"SpellE\">of<\/span> muscovite, biotite, <span class=\"SpellE\">chlorite<\/span>, and ilmenite.<\/span> <span class=\"Apple-style-span\"><span class=\"SpellE\">Temperatures<\/span> up <span class=\"SpellE\">to<\/span> 595 \u00b0C and <span class=\"SpellE\">pressures<\/span> up <span class=\"SpellE\">to<\/span> 0.67 <span class=\"SpellE\">GPa<\/span> <span class=\"SpellE\">have<\/span> <span class=\"SpellE\">been<\/span> <span class=\"SpellE\">reported<\/span> <span class=\"SpellE\">by<\/span><span class=\"SpellE\">Franceschelli<\/span> <span class=\"SpellE\">et<\/span> al. (1989), and <span class=\"SpellE\">pressures<\/span> <span class=\"SpellE\">over<\/span> 0.9 <span class=\"SpellE\">GPa<\/span> <span class=\"SpellE\">by<\/span> <span class=\"SpellE\">Carosi<\/span> & <span class=\"SpellE\">Palmeri<\/span> (2002) <span class=\"SpellE\">for <\/span>the <span class=\"SpellE\">metamorphic<\/span> <span class=\"SpellE\">peak<\/span><\/span>.<\/p>\n","modified":"2018-09-03T17:41:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/ky-2-1024x1024.jpg","taxonomy":{"webmapp_category":[234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5745","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5745&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/kyanite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.579414000000043,40.6018154]}},{"type":"Feature","properties":{"id":5744,"name":"S-C-C’ fabric in orthogneiss","description":"<p>S-C-C’ fabric in Ordovician orthogneiss, top-to-the NE sense of shear and thin section photo (II nicols).<\/p>\n<p><span class=\"Apple-style-span\">On the road near of \u00abCantoniera Mt. Tundu\u00bb we start to see outcorps of granodioritic orthogneiss with a prominent C-S fabric and C\u2019 structures pointing to a top-to-the NW sense of shear (\u201cdextral\u201d)<\/span>.<\/p>\n","modified":"2018-09-03T18:04:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/S-Cogn-1024x768.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5744","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5744&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/s_c-fabric-in-orthogneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.598055599999952,40.5950246]}},{"type":"Feature","properties":{"id":5743,"name":"Garnet + staurolite bearing micaschist","description":"<p><span class=\"Apple-style-span\">On the road <span class=\"SpellE\">from<\/span> <span class=\"SpellE\">Torp\u00e8<\/span> <span class=\"SpellE\">village<\/span> <span class=\"SpellE\">to<\/span> <span class=\"SpellE\">Lod\u00e8<\/span> (S. Anna <span class=\"SpellE\">villages<\/span>) <span class=\"SpellE\">there<\/span> <span class=\"SpellE\">is<\/span> <span class=\"SpellE\">an<\/span> <span class=\"SpellE\">outcorp<\/span> <span class=\"SpellE\">of<\/span> staurolite and <span class=\"SpellE\">garnet<\/span> <span class=\"SpellE\">bearing<\/span> <span class=\"SpellE\">micaschist<\/span>: <span class=\"SpellE\">near<\/span> the <span class=\"SpellE\">gate<\/span> at the <span class=\"SpellE\">entrance<\/span> <span class=\"SpellE\">of<\/span> a <span class=\"SpellE\">small<\/span> <span class=\"SpellE\">forest<\/span> <span class=\"SpellE\">track<\/span>, <span class=\"SpellE\">we<\/span> <span class=\"SpellE\">see<\/span> <span class=\"SpellE\">cm-size<\/span>staurolite and <span class=\"SpellE\">garnet<\/span> <span class=\"SpellE\">porphyroclasts<\/span> on the S2 <span class=\"SpellE\">foliation<\/span> <span class=\"SpellE\">of<\/span> the <span class=\"SpellE\">micaschist. Garnet and staurolite grew after the D1 and from pre-to syn-D2 deformation phase.<\/span> <\/span><\/p>\n","modified":"2018-09-03T18:03:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/Garnetstaurolite-bearing-micaschist-300x300.png","taxonomy":{"webmapp_category":[234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5743","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5743&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/garnetstaurolite-bearing-micaschist\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.579414000000043,40.6018154]}},{"type":"Feature","properties":{"id":5741,"name":"Orthogneiss","description":"<p>Deformed mafic microgranular enclave in the sheared Ordovician granodioritic orthogneiss.<\/p>\n","modified":"2018-12-12T09:38:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/08\/Ortogneiss-1024x770.png","taxonomy":{"webmapp_category":[234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/5741","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=5741&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/orthogneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.53913799999998,40.591026]}},{"type":"Feature","properties":{"id":2304,"name":"\u03c3-type porphyroclast","description":"<p>\u03c3-type porphyroclast of K-feldspar in the strongly sheared augengneisses of the Aiguilles Rouges Massif. Dextral sense of shear. 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The Vale da<br \/>\nLua is well preserved and to keep this condition it is necessary to increase the information to the visitors about<br \/>\nthe rocks conditions formation (including depositional and sedimentary processes), once there is great confusion<br \/>\nby part of the public, and many believe in volcanic origin to the local rocks. It is important to emphasize in<br \/>\nwarning plates, the importance of the area preservation, the prohibition of getting rock samples and the general<br \/>\nmaintenance of the place. PhotoID801<\/p>\n<p>Photograph:<\/p>\n<p>Reference: Campos,J.E.G.; Monteiro,C.F.; Dardenne,M.A. 2005. S\u00e3o Miguel Conglomerate in the Vale da Lua valley, South of the Chapada dos Veadeiros Park, State of Goi\u00e1s, Brazil – Beautiful exotic scenario modeled by fluvial erosion. In: Winge,M.; Schobbenhaus,C.; Berbert-Born,M.; Queiroz,E.T.; Campos,D.A.; Souza,C.R.G. ; Fernandes,A.C.S. (Edit.) Geological and Palaeontological Sites of Brazil. Available on line 13\/6\/2005 at the address http:\/\/www.unb.br\/ig\/sigep\/sitio077\/sitio077english.pdf<\/p>\n","modified":"2018-07-24T12:25:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Vale-da-Lua-768x370.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2274","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2274&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/vale-da-lua\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-47.789652943611,-14.18700309228]}},{"type":"Feature","properties":{"id":2272,"name":"Cm-scale graben, Khabr mountain","description":"<p>Caption: Graben is the downthrown part of rock within extensional tectonics such as rifts.<br \/>\nGrabens are commonly bound by horsts and can be formed in a linear,<br \/>\nnon-linear or radial (as collapse crater) style at different geological scales. The<br \/>\nphotograph shows two oppositely dipping normal faults forming a spectacular cm-scale graben.<br \/>\nThis structure formed within the sequence of Devonian alternating layers of calc-schist, metalimestone<br \/>\nturbidite (brown) and thin bands of laminated marble (white). Metamorphic units is<br \/>\nresult from Early Cimmerian orogeny. No drag of the faulted unit characterizes it as a specific<br \/>\ntype of flanking structure. The throw (vertical displacement) on the fault is ~2 cm (follow the marker layer).<br \/>\nExtensional faulting within compressional orogeny is a crux and attracts geologists.<br \/>\nExtensional tectonism and its related structures may occur during as well as after the<br \/>\ncontractional history of a collisional orogeny. It is important in structural analysis and tectonic<br \/>\nmodelling to know which structures are synorogenic and which formed during the postcontractional stage. Synorogenic extensional structures are related to orogeny-internal<br \/>\nfeatures that cause relatively local instabilities in an overall contractional regime. By contrast<br \/>\nsignificant postorogenic extensional deformation implies true extension at the scale of the<br \/>\norogenic belt and crust. Accordingly, orogeny can be affected by<br \/>\ncontractional and extensional deformations overprinting each other and producing complex<br \/>\nstructural architectures (such as type-II superposed folds). Small-scale extension is commonly<br \/>\nrelated to local thrust faults and brittle-ductile shear zones. From the Khabr Mountain.<br \/>\nStructural zone of Sanandaj-Sirjan metamorphic-ophiolitic Complex, SW of the city of Baft,<br \/>\nKerman province, Iran (Location 28\u00b052\u00b404\u02baN, 56\u00b023\u00b456\u02baE). The coin radius is 1.25 cm. PhotoID800<\/p>\n<p>Photograph: Seyed Tohid Nabavi<\/p>\n","modified":"2018-06-30T13:04:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cm-scale-graben-Khabr-mountain-768x439.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2272","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2272&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/cm-scale-graben-khabr-mountain\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[56.41699215397239,28.83986196550162]}},{"type":"Feature","properties":{"id":2268,"name":"Slump folding in the Karaj Formation","description":"<p>Folds caused by gravitational gliding in unconsolidated and soft-sediments are called slump folds. They can form by layer-parallel shear. Such folds reflect the orientation of the palaeoslope in ancient settings. PhotoID799<br \/>\nThe photograph was taken from the road section of Eocene Karaj Formation, near Karaj city (with a view to the WNW), 35\u00b0 50\u00b4 11\u02ddN, 51\u00b0 02\u00b4 40\u02ddE. Karaj Formation, ~ 3300 m thick, mainly composed of a heterogeneous assemblage of green tuff and tuffite, thin bands of marine shale, and igneous rocks. The thick turbidites with slump folding in the Karaj Formation may indicate a relatively deep water through and submarine fan. The Z-shaped asymmetric and overturned slump fold indicate northward palaeoslope. These conditions show stage 3 geometries (late translation of slump) of formation and develop of slump fold system by surging flow with flow accelerates and contraction increases downslope.<\/p>\n<p>Photograph: Seyed Tohid Nabavi<\/p>\n","modified":"2018-10-10T18:32:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Slump-folding-in-the-Karaj-Formation-768x441.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2268","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2268&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/slump-folding-in-the-karaj-formation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[50.966125490376726,35.85010031851634]}},{"type":"Feature","properties":{"id":2266,"name":"Rotated Staurolite","description":"<p>Rotated Staurolite with quartz asymmetric tails in the Staurolite-bearing micaschists of the Maures-Tanneron Massif (external zone). 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PhotoID798<\/p>\n<p>Photograph: Matteo Simonetti<\/p>\n","modified":"2018-06-15T10:31:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rotated-Staurolite-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2266","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2266&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/rotated-staurolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.474844241523783,43.16923805984651]}},{"type":"Feature","properties":{"id":2264,"name":"Sibuti Formation Miri","description":"<p>The excellent field exposure of a large thrust fault observed in Sibuti Formation, Miri Sarawak Malaysia. Backthrust are beautifully preserved in the thrust-wedge on the hanging wall of the large fault. PhotoID797<\/p>\n<p>Photograph: Batmanathan Navakanesh<\/p>\n<p>Reference: Batmanathan Navakanesh, Mohammed Khalil, Nur Aqilah Safar, Praviandy Gustandika., Structural Analysis of Miri-Beluru region, Sarawak, Malaysia. Final Year Project for B.Sc. Applied Geology, 2015, Curtin Sarawak Malaysia. Advisor: Dr. Afroz Shah<\/p>\n","modified":"2018-06-30T19:56:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sibuti-Formation-Miri-768x567.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2264","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2264&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/sibuti-formation-miri\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[113.94599,4.02422]}},{"type":"Feature","properties":{"id":2262,"name":"Rainy Cove Angular Unconformity","description":"<p>A classic angular unconformity, testimony to initial continental break-up<br \/>\nPhotoID796<\/p>\n<p>Photograph: Elisabeth Kosters<\/p>\n<p>Reference: http:\/\/earthsciencesociety.com\/2015\/01\/03\/nova-scotias-own-great-unconformity-my-new-banner-photo-for-2015\/<\/p>\n","modified":"2018-09-04T12:28:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rainy-Cove-Angular-Unconformity-768x245.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2262","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2262&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/rainy-cove-angular-unconformity\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[64.04,45.13]}},{"type":"Feature","properties":{"id":2260,"name":"Carua\u00e7u Member – Maracangalha Formation","description":"<p>Succession of fine to medium sandstone showing hummocky cross stratification, tool marks and parts of Bouma sequence. There are also normal and reverse faults in the outcrop. This member is the register of turbidity flow in a lacustre system<br \/>\nPhotoID795<\/p>\n<p>Photograph: Guilherme Duarte<\/p>\n<p>Reference: Magnavita et al 2005 – Guia de Campo da Rec\u00f4ncavo, NE do Brasil<\/p>\n","modified":"2018-10-10T18:33:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Carua\u00e7u-Member-Maracangalha-Formation-577x1024.jpg","taxonomy":{"webmapp_category":[220,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2260","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2260&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/caruacu-member-maracangalha-formation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-38.6162862182,-12.9298916864]}},{"type":"Feature","properties":{"id":2258,"name":"Salta Group veins","description":"<p>Salta Group Yacoraite Formation calcite veins limestone<br \/>\nPhotoID794<\/p>\n<p>Photograph: John Hooker<\/p>\n","modified":"2018-09-04T11:19:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Salta-Group-veins-768x576.jpg","taxonomy":{"webmapp_category":[224]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2258","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2258&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/salta-group-veins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-65.48,-22.98]}},{"type":"Feature","properties":{"id":2256,"name":"K7T Boundary at Barrranco del Gredero,","description":"<p>K\/T boundary layer (Thin yellow layer below dark bed) in the Barranco de El Gredero Section, Caravaca, Spain.<br \/>\nPhotoID792<\/p>\n<p>Photograph: Enrique Bern\u00e1rdez Rodr\u00edguez<\/p>\n<p>Reference: MOLINA, E., (2004). Eventos de extinci\u00f3n del Cret\u00e1cico-Terciario: valor patrimonial y conservaci\u00f3n del barranco del Gredero (Caravaca, Murcia), en El Patrimonio Geol\u00f3gico: Cultura, Turismo y Medio Ambiente (F. Guill\u00e9n Mond\u00e9jar y Antonio del Ramo Jim\u00e9nez, eds.). Dpto. de Geolog\u00eda, Univ. de Murcia, 41-49.<\/p>\n","modified":"2018-06-30T12:42:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/K7T-Boundary-at-Barrranco-del-Gredero-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2256","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2256&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/k7t-boundary-at-barrranco-del-gredero\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-1.87809348106,38.07668919966185]}},{"type":"Feature","properties":{"id":2252,"name":"Hercinian folds in Ballota Beach","description":"<p>Fold propagation and fautt bend folds in red mudastones from the Tournaisian- Visean Alba Formation in Ballota Beach, Llanes, Asturias, Northern Spain.<br \/>\nPhotoID791<\/p>\n<p>Photograph: Enrique Bern\u00e1rdez Rodr\u00edguez<\/p>\n","modified":"2018-09-04T11:12:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Hercinian-folds-in-Ballota-Beach-768x576.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2252","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2252&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/hercinian-folds-in-ballota-beach\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.71158981323,43.411844042307344]}},{"type":"Feature","properties":{"id":2250,"name":"Goodland Formation – White Settlement","description":"<p>This is an exposure along a creek east of the end of Roe St., White Settlement, Texas.<br \/>\ntaken Feb. 21, 2010.<br \/>\nPhotoID790<\/p>\n<p>Photograph: Lance Hall<\/p>\n","modified":"2018-06-30T11:09:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Goodland-Formation-White-Settlement-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2250","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2250&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/goodland-formation-white-settlement\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-97.453387,32.758382]}},{"type":"Feature","properties":{"id":2248,"name":"Duck Creek Formation – Fort Worth","description":"<p>This is an exposure of the Duck Creek Formation in an old quarry NE of the intersection of Old Decator Rd and Hwy 820, Fort Worth, Texas. 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Mountains Garnetite (Close-up)","description":"<p>Close-up of garnet crystals in the garnetite layer.<br \/>\nPhotoID762<\/p>\n<p>Photograph: Ben Murphy<\/p>\n","modified":"2018-09-04T11:26:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bradshaw-Mountains-Garnetite-Close-up-768x576.jpg","taxonomy":{"webmapp_category":[234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2200","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2200&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/bradshaw-mountains-garnetite-close-up\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-112.35401,34.18239]}},{"type":"Feature","properties":{"id":2198,"name":"Bradshaw 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La scienza della Terra nell\u2019area della provincia di Livorno a sud del fiume Cecina \u2013 Quaderni del museo di Storia Naturale di Livorno \u2013 vol.13 (1993) Supplemento n.2 -DECANDIA F.A., LAZZAROTTO A., LIOTTA D., Structural features of southern Tuscany, Italy \u2013 Ofioliti, 26 (2a), 287-300, 2001.<\/p>\n","modified":"2018-10-10T18:39:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Veins-sedimentary-into-the-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2168","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2168&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/veins-sedimentary-into-the\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.640256106853485,43.08193039638786]}},{"type":"Feature","properties":{"id":2166,"name":"Recumbent folds","description":"<p>Minor recumbent F1 west-facing folds in the hinge zone of La Spezia megafold affecting the Tuscan Nappe. Red layers are in Diaspri Formation (cherts) whereas withish layers are in the Maiolica Formation (limestone).<br \/>\nPhotoID741<\/p>\n<p>Photograph: C. Montomoli, R. Carosi<\/p>\n<p>Reference: Montomoli C., Ruggeri G., Boiron M. C., Cathelineau M. (2001) – Pressure fluctuation during uplift of the Northern Apennines (Italy): a fluid inclusion study. Tectonophysics, 314, 121-139. Montomoli C. (2002) – Vein development and fluid inclusion data: insight on the evolution of the Tuscan Nappe in the Northern Apennines. Boll. Soc. Geol. It.\/Italian Journal of Geoscience, 801-817. Carosi R., Leoni L., Montomoli C., Sartori F. (2003) – Very low-grade metamorphism in the Tuscan Nappe, Northern Apennines, Italy: relationships between deformation and metamorphic indicators in the La Spezia mega-fold. Schweiz. Schweiz. 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Kamil Crater has rim to rim diameter of 45 m. It was generated by the hypervelocity impact of the Gebel Kamil iron meteorite. Note simple crater structure and prominent ejecta ray pattern. For its exceptional pristine status, Kamil Crater is considered a model crater for small-scale impacts on Earth. Photo ID 628<\/p>\n<p>Photograph:<\/p>\n<p>Reference: Folco L. et al. (2010) The Kamil Crater in Egypt. Science 329, 804. Folco L. et al. (2011) Kamil Crater (Egypt): ground truth for small scale meteorite impact on Earth. Geology 39, 179-182. D\u2019Orazio M. et al. (2011) Gebel Kamil: the iron meteorite that formed the Kamil Crater (Egypt). Meteoritics and Planetary Science 46, 1179 -1196.<\/p>\n","modified":"2018-06-28T14:48:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kamil-Crater-768x851.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2035","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2035&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/kamil-crater\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[26.08768750190734,22.018314574874932]}},{"type":"Feature","properties":{"id":2033,"name":"ductile shear zone, Swaziland","description":"<p>Ductile shear zone in tonalitic gneiss<\/p>\n<p>Photograph: Sebastian Schr\u00f6der and Nils Suhr<\/p>\n","modified":"2018-06-30T10:53:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/ductile-shear-zone-Swaziland-225x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2033","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2033&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/ductile-shear-zone-swaziland\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[31.3913,-26.825516]}},{"type":"Feature","properties":{"id":1257,"name":"Mylonite, Monashee Complex","description":"<p>Mylonites in upper shear zones of the Monashee Metamorphic Complex: top-down to-the-east sense of shear. 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Geological Association of Canada, Cordilleran Section, 165 pp.<\/p>\n","modified":"2019-02-12T06:25:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonite-Monashee-Complex-768x516.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1257","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1257&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mylonite-monashee-complex\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.97011967881195,50.82090872350237]}},{"type":"Feature","properties":{"id":1191,"name":"McConnel Thrust","description":"<p>McConnel thrust; Mount Yamnuska. 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Geological Association of Canada, Cordilleran Section, 165 pp.<\/p>\n","modified":"2018-06-28T13:28:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/McConnel-Thrust-768x516.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1191","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1191&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mcconnel-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-115.065366,51.085712]}},{"type":"Feature","properties":{"id":1114,"name":"veins in gneiss","description":"<p>Archaean gneiss with complex vein system<\/p>\n<p>Photograph: Sebastian Schr\u00f6der and Nils Suhr<\/p>\n","modified":"2018-09-03T17:56:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/veins-in-gneiss-768x576.jpg","taxonomy":{"webmapp_category":[234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1114","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1114&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/veins-in-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[30.734671,-27.033955]}},{"type":"Feature","properties":{"id":2067,"name":"Columnar basalts in Guspini","description":"<p>Spectacular Pliocene columnar basalts in a quarry in Guspini, Sardinia. The outcrop is in a private graden, ask for permission before entering.<\/p>\n<p>See<br \/>\nhttp:\/\/www.parcodessi.it\/parcodessi\/export\/sites\/default\/inglese\/Schedario\/Immagini\/basaltiColonnari01g.jpg<\/p>\n<p>Photograph:<\/p>\n","modified":"2018-12-13T17:27:35","color":"","icon":"","noDetails":false,"noInteraction":false,"taxonomy":{"webmapp_category":[224]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2067","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2067&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/columnar-basalts-in-guspini\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.635125160217285,39.539131207210374]}},{"type":"Feature","properties":{"id":2031,"name":"tonalitic gneiss","description":"<p>Archaean tonalitic gneiss, strongly deformed with remains of mafic dykes, cut by several sets of pegmatite and granite veins, and ductile and brittle shear zones. 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Milano, Jan. 1986.<\/p>\n","modified":"2018-06-30T11:44:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/brittle-ductile-shear-zone-on-ice-flow-768x518.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2027","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2027&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/brittle-ductile-shear-zone-on-ice-flow\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[164.90684509277344,-73.4722354479]}},{"type":"Feature","properties":{"id":2025,"name":"Silicified fault breccia\/gouge","description":"<p>Field photograph of a silicified fault breccia\/gouge zone in sheared granitoids of Gavilgarh-Tan shear zone, central India. The faults are roughly East-West and generally parallel to the mylonitic foliation in granitoids. Mylonitic foliation is clearly seen in the large fragments of host rock within the silicified zone. At places, such faults have displaced Deccan Trap lava flows, and therefore should be post-Mesozoic in age. Photo ID 615<\/p>\n<p>Photograph: A. Chattopadhyay, University of Delhi.<\/p>\n","modified":"2018-07-24T15:56:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Silicified-fault-brecciagouge-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2025","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2025&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/silicified-fault-breccia-gouge\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[76.46426169999995,21.04131989999999]}},{"type":"Feature","properties":{"id":2023,"name":"Angular unconformity","description":"<p>An angular unconformity between folded Jurassic chert and chertly limestone beds of the Pindos Nappe (below) and Pliocene coastal deposits (above); the unconformity level is about 4m above the present day sea level (Kythira Island). 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Zeitschrift der Deutschen Gesellschaft f\u00fcr Geowissenschaften, 159, 439-455.<\/p>\n","modified":"2018-06-30T11:09:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Angular-unconformity-1-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2023","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2023&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/angular-unconformity-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[22.923232,36.286808]}},{"type":"Feature","properties":{"id":2021,"name":"Metaconglomerate","description":"<p>Strongly deformed metaconglomerate layer of the Phyllite-Quartzite unit (Lower high-pressure nappes, External Hellenides). 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Geological Society, London, Special Publications, 268, 497-516.<\/p>\n","modified":"2018-06-30T11:36:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Metaconglomerate-768x576.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2021","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2021&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/metaconglomerate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[22.255174,37.090057]}},{"type":"Feature","properties":{"id":2017,"name":"Als\u00f3telekes, gypsum open pit","description":"<p>Folds in laminar gypsum.<br \/>\nThe mine is located on a gypsum-anhydrite dome structure with sheath folds and other flow structures in a regional strike-slip fault zone (Darn\u00f3 Zone) Photo ID 612<\/p>\n<p>Photograph: N\u00e9meth Norbert<\/p>\n<p>Reference: ZELENKA T. \u2013 KAL\u00d3 J. \u2013 N\u00c9METH N. 2005: Az als\u00f3telekesi gipsz-anhidrit d\u00f3m szerkezete. 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The 1538 Monte Nuovo eruption (Campi Flegrei, Italy). Bulletin of Volcanology 49, 608-615<\/p>\n","modified":"2018-10-08T11:42:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Monte-Nuovo-1-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1889","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1889&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/monte-nuovo-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.083507061004639,40.836411420089426]}},{"type":"Feature","properties":{"id":2013,"name":"Diabase intrusion with Greenstone","description":"<p>Diabase intrusion into greenstone with some greenstone clasts along side trail out to Point Bonita. 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Metamorphic Geology, 26, 403-426.<\/p>\n","modified":"2018-06-30T12:24:51","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Migmatitic-gneisses-768x576.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1875","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1875&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/migmatitic-gneisses\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.374256134033203,41.67215850558213]}},{"type":"Feature","properties":{"id":1857,"name":"Basalt Dyke","description":"<p>Basalt Dyke in the Rognano Ophiolite<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-09-04T11:26:57","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Basalt-Dyke-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1857","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1857&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/basalt-dyke\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.454521179199219,43.47422444431377]}},{"type":"Feature","properties":{"id":1855,"name":"Monzogranite mylonite","description":"<p>Monzogranite mylonite intruded in the sinistral (top-to-the West) shear zone in the anphibolitic metamorphic complex. From Punta Chiappa, SE Corsica.<\/p>\n<p>Photograph: D. Pieruccioni<\/p>\n<p>Reference: Giacomini et al. (2008): Exhumation of a Variscan orogenic complex: insights into the composite granulitic\u2013amphibolitic metamorphic basement of south-east Corsica (France). J. Metamorphic Geology, 26, 403-426.<\/p>\n","modified":"2018-07-24T11:39:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Monzogranite-mylonite-768x1024.jpg","taxonomy":{"webmapp_category":[232,234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1855","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1855&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/monzogranite-mylonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.368183612823486,41.596148735352934]}},{"type":"Feature","properties":{"id":1853,"name":"synsedimentary fault","description":"<p>Synsedimentary fault in Rosso Ammonitico Fm. 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(the height of the cut is about 6 m)<\/p>\n<p>Photograph: F.Milazzo<\/p>\n","modified":"2018-06-30T11:45:29","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/synsedimentary-fault-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1853","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1853&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/synsedimentary-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.394268035888672,44.181665379510186]}},{"type":"Feature","properties":{"id":1851,"name":"shear band in Erabiddy shear zone","description":"<p>Hornblende-granitoid with steep foliation and layering (trending E-W) and a subvertical stretching lineation (not visible), cut by D2-shear bands that indicate N-side up (N at right). 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Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga). North at the top<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-09-03T17:46:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Migmatic-gneiss-768x502.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1827","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1827&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/migmatic-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.381667,-25.582667]}},{"type":"Feature","properties":{"id":1825,"name":"shear band with melt","description":"<p>Banded gneiss with melt vein in a shear band. 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The deformation is of unknown age, but may be the steep deformation component of the Errabiddy shear zone. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga). 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The deformation is of unknown age, but may be the steep deformation component of the Errabiddy shear zone. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:37:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-Gneiss-2-768x502.jpg","taxonomy":{"webmapp_category":[234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1821","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1821&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/yarweelor-gneiss-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.53419493121339,-25.5681515857]}},{"type":"Feature","properties":{"id":1819,"name":"Yarweelor Gneiss","description":"<p>Grey gneiss that has strongly deformed mafic bands, several generations of granitic veins and sinistral shear bands with leucosome material. 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Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T19:18:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-Gneiss-1-768x502.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1819","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1819&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/yarweelor-gneiss-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.53487084788514,-25.5688242179]}},{"type":"Feature","properties":{"id":1809,"name":"Pencil cleavage","description":"<p>Pencil cleavage in wm-chl phyllite. Camel Hills metasediments, (ca. 2000 Ma).<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:23:42","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pencil-cleavage-768x502.jpg","taxonomy":{"webmapp_category":[232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1809","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1809&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/pencil-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.654667,-25.533]}},{"type":"Feature","properties":{"id":1805,"name":"Camel Hills","description":"<p>View of the Camel Hills, composed of Camel Hills metasediments (ca. 2000 Ma)<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T19:25:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Camel-Hills-768x494.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1805","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1805&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/camel-hills\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.533155,-25.580881]}},{"type":"Feature","properties":{"id":1803,"name":"Dalgaringa gneiss","description":"<p>Dalgaringa Supersuite (c. 1985) – intrusive into the Glenburg Terrane. This suite is intrusive into the Halfway gneiss north of the Errabiddy shear zone, and may be subduction related and formed during the Glenburg orogeny. The gneiss is moderately-strongly deformed with EW trending foliations and gently W-plunging stretching lineations.<br \/>\nThe pavements show banded gneiss intruded by less deformed granite pegmatite veins. North at the top<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:27:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dalgaringa-gneiss-2-768x496.jpg","taxonomy":{"webmapp_category":[229,232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1803","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1803&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/dalgaringa-gneiss-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.57345061111448,-25.5129526909]}},{"type":"Feature","properties":{"id":1871,"name":"Capo Bianco aplite","description":"<p>Contact between Capo bianco Aplite and Ryolite.<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-30T12:25:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Capo-Bianco-aplite-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1871","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1871&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/capo-bianco-aplite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.317057967185974,42.81951211922519]}},{"type":"Feature","properties":{"id":1861,"name":"Ammonite","description":"<p>Ammonite in the rosso ammonitico formation<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-28T18:17:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Ammonite-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1861","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1861&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/ammonite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.383110046386719,44.20017426009329]}},{"type":"Feature","properties":{"id":1785,"name":"Yarweelor augengneiss","description":"<p>Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga). 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Looking NE<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:47:14","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/veins-in-TTG-gneiss-768x502.jpg","taxonomy":{"webmapp_category":[224]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1815","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1815&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/veins-in-ttg-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.534667,-25.5685]}},{"type":"Feature","properties":{"id":1642,"name":"Rosignano ophiolite","description":"<p>Basaltic dyke in Rosignano Ophiolite (Gabbro)<br \/>\nPhotoID382<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-07-24T11:41:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rosignano-ophiolite-1-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1642","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1642&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/rosignano-ophiolite-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.435638427734375,43.43696596521823]}},{"type":"Feature","properties":{"id":1640,"name":"Rosignano ophiolite","description":"<p>Basaltic dyke in Rosignano Ophiolite<br \/>\nPhotoID381<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-30T11:11:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rosignano-ophiolite-768x301.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1640","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1640&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/rosignano-ophiolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.435638427734375,43.43696596521823]}},{"type":"Feature","properties":{"id":1813,"name":"migmatic veins","description":"<p>Migmatitic gneiss with melt veins axial planar to older melt veins which have been folded; the last veins are deformed by the Errabiddy shear zone mylonites. Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga)<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T11:43:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/migmatic-veins-768x493.jpg","taxonomy":{"webmapp_category":[224,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1813","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1813&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/migmatic-veins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.7945,-25.544333]}},{"type":"Feature","properties":{"id":1811,"name":"Yalbra Hill","description":"<p>View from Yalbra Hill (Mt James Formation conglomerates) to the east over the northern part of the Yilgarn craton; the outcrops of the Errabiddy shear zone are in the brown patch at left<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:47:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yalbra-Hill-768x502.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1811","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1811&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/yalbra-hill\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.230833,-25.686333]}},{"type":"Feature","properties":{"id":1807,"name":"Camel Hills folded metapelite","description":"<p>Metapelite alternating with quartzite , looking West (north at the right). There is a strong stretching lineation on steeply N dipping foliation surfaces; Lstr 167-79. Camel Hills metasediments, (ca 2000 Ma).<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T16:14:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Camel-Hills-folded-metapelite-196x300.jpg","taxonomy":{"webmapp_category":[229,232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1807","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1807&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/camel-hills-folded-metapelite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.384,-25.601167]}},{"type":"Feature","properties":{"id":1801,"name":"Dalgaringa gneiss","description":"<p>Dalgaringa Supersuite (c. 1985) – intrusive into the Glenburg Terrane. This suite is intrusive into the Halfway gneiss north of the Errabiddy shear zone, and may be subduction related and formed during the Glenburg orogeny. The gneiss is moderately-strongly deformed with EW trending foliations and gently W-plunging stretching lineations.<br \/>\nThe pavements show banded gneiss rafts in younger less deformed granite pegmatite veins. North at the top<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:45:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dalgaringa-gneiss-1-768x502.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1801","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1801&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/dalgaringa-gneiss-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.573,25.512333]}},{"type":"Feature","properties":{"id":1638,"name":"Finero","description":"<p>Finero Peridotite (Olivine, Phlogopite, Cr-Diopside); Lithosferic mantel affected by metasomatsm.<br \/>\nPhotoID379<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-09-04T15:55:32","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Finero-1-768x576.jpg","taxonomy":{"webmapp_category":[234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1638","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1638&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/finero-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.531227111816406,46.102637544820595]}},{"type":"Feature","properties":{"id":1799,"name":"Dalgaringa gneiss","description":"<p>Dalgaringa Supersuite (c. 1985) – intrusive into the Glenburg Terrane. This suite is intrusive into the Halfway gneiss north of the Errabiddy shear zone, and may be subduction related and formed during the Glenburg orogeny. The gneiss is moderately-strongly deformed with EW trending foliations and gently W-plunging stretching lineations. The pavements show banded Dalgaringa gneiss cut by several generations of granite and pegmatite veins, possibly of Wooramel and Moorarie age. West at the top. S 178-82; Lstr 253-32<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-07-24T12:18:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dalgaringa-gneiss-768x502.jpg","taxonomy":{"webmapp_category":[234,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1799","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1799&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/dalgaringa-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.57327894973753,-25.5128364991]}},{"type":"Feature","properties":{"id":1797,"name":"Halfway gneiss","description":"<p>Weakly deformed dark gneiss with an age of 2550Ma, intruded by veins of 2000 Ma granite – both constitute the Halfway gneiss when deformed<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:47:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Halfway-gneiss-768x497.jpg","taxonomy":{"webmapp_category":[224]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1797","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1797&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/halfway-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.01745,-25.10295]}},{"type":"Feature","properties":{"id":1795,"name":"Moorarie Granite","description":"<p>Undeformed granite, probably Moorarie (ca 1830-1780 Ma). There are shear zones in the granite locally, but these have only vertical lineations, never horizontal ones; the horizontal lineations seem to be cut by the Moorarie granites. I therefore interpret the Moorarie suite to intrude during the first and second phases of activity on the Errabiddy shear zone<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:43:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Moorarie-Granite-768x502.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1795","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1795&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/moorarie-granite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.629,-25.550667]}},{"type":"Feature","properties":{"id":1636,"name":"Finero peridotite","description":"<p>Finero Peridotite (Olivine, Phlogopite, Cr-Diopside); Lithosferic mantel afffected by metasomatism.<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-30T12:28:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Finero-peridotite-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1636","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1636&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/finero-peridotite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.536205291748047,46.10192339248404]}},{"type":"Feature","properties":{"id":1241,"name":"Serpentine along Hayward fault","description":"<p>Masses of ophiolites, serpentinized mafic material that are remnants of ancient oceanic crust, outcrop along the Hayward fault zone. Photo ID 712<\/p>\n<p>Photograph: David Manaker<\/p>\n","modified":"2018-09-04T13:23:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Serpentine-along-Hayward-fault-768x513.jpg","taxonomy":{"webmapp_category":[220,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1241","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1241&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/serpentine-along-hayward-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-122.178909,37.805243]}},{"type":"Feature","properties":{"id":1793,"name":"sheath folds in quartzite","description":"<p>Strongly mylonitised vein-quartzite with D2-sheath folds. Foldaxes are strongyl curved and both vertical and horizontal orientations are visible. A strong stretching lineation is folded over the sheath folds, probably formed earlier during D2 in the Erabiddy shear zone.<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:36:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sheath-folds-in-quartzite-196x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1793","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1793&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/sheath-folds-in-quartzite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.381333,-25.6015]}},{"type":"Feature","properties":{"id":1791,"name":"stretching lineation in quartzite","description":"<p>Strongly mylonitised vein-quartzite in the Erabiddy shear zone, with steeply south-dipping foliation and very strong subvertical D2-stretching lineation<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T13:05:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/stretching-lineation-in-quartzite-768x500.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1791","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1791&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/stretching-lineation-in-quartzite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.381,-25.6015]}},{"type":"Feature","properties":{"id":1789,"name":"Double stretching lineations","description":"<p>Vertical E-W trending foliation surface of Yarweelor bi-granite gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga) showing two lineations: one stretching lineation (vague striping) plunging gently (14\u00b0) to the east (left) and one biotite mineral lineation plunging steeply ( 60\u00b0) to the east (left). The latter lineation is parallel to elliptical aggregates of biotite which may represent pseudomorphs after another mineral (garnet?). In that case, this unknown mineral must have predated the steep lineation, which would therefore be the younger one of the two. The gently lineation is interpreted as D1: the steep one as D2. The D1-lineation is best visible at the top and bottom of the photograph. Vertical outcrop surface. The two lineations are thought to represent the two phases of activity of the Erabiddy shear zone.<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:10:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Double-stretching-lineations-768x502.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1789","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1789&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/double-stretching-lineations\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.381667,-25.585667]}},{"type":"Feature","properties":{"id":1787,"name":"Mylonitised calcsilicate","description":"<p>Mylonitised calcsilicate of the Camel Hills metasediments ( ca. 2000 Ma) in the Erabiddy shear zone. The fabric is a strong vertical stretching lineation parallel to foldaxes. The folds may be original D1-drag folds, stretched during D2. The lineation is interpreted as a D2-structure. These are two phases in the activity of the Erabiddy shear zone.<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:41:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitised-calcsilicate-192x300.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1787","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1787&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mylonitised-calcsilicate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.809833,-25.495]}},{"type":"Feature","properties":{"id":1783,"name":"shear bands in calcsilicate","description":"<p>Calcsilicates (top and bottom) of the Camel Hills metamorphics, with an age of appr. 2000 Ma. The deformation fabric is a weak steep foliation and weak subhorizontal E-W trending lineation in calcsilicate. A granite vein (centre) is affected by ductile dextral D1-shear bands, which grade into brittle dextral shear fractures in the calcsilicate. Granite is of Wooramel or Moorarie age. 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Width of view 30 cm<br \/>\nPhotoID475<\/p>\n<p>Photograph: Cees 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shape flame in Peperino Ignimbrite<br \/>\nPhotoID374<\/p>\n<p>Photograph: Alessandro Da 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The mylonites define the decollement of the Wadi Sikeit core complex.<br \/>\nPhotoID365<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:49:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/folded-mylonites-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1620","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1620&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/folded-mylonites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[34.79671061038971,24.63022903917177]}},{"type":"Feature","properties":{"id":1618,"name":"Hafafit decollement","description":"<p>View to the east of the gently N-dipping mylonites of the Hafafit core complex decollement. The movement is extensional, top to the left in the image.<br \/>\nPhotoID364<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-09-04T13:31:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Hafafit-decollement-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1618","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1618&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/hafafit-decollement\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[34.44145202636719,24.810576840999975]}},{"type":"Feature","properties":{"id":1616,"name":"Cambrian Unconformity","description":"<p>Cambrian sandstone overlying grey granite of 600-620 Ma, which is intruded by 580Ma red granite. 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Marker indicates viewpoint of photographer, looking east<br \/>\nPhotoID362<\/p>\n<p>Photograph: Cees Passchier, Ghaleb Jarrar<\/p>\n","modified":"2018-09-04T13:28:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Wadi-Rahma-dykes-1-768x576.jpg","taxonomy":{"webmapp_category":[234,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1614","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1614&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/wadi-rahma-dykes-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[35.15118598937988,29.90788738182232]}},{"type":"Feature","properties":{"id":1600,"name":"Sheath fold – eye fold","description":"<p>Eye folds. Port Vasgo, Scotland<br \/>\nPhotoID356<\/p>\n<p>Photograph: Jim Talbot<\/p>\n<p>Reference: See more photos at: http:\/\/myweb.facstaff.wwu.edu\/talbot\/cdgeol\/Localities\/Sheath.html#Portvasgo<\/p>\n","modified":"2018-06-30T11:20:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-fold-eye-fold-768x495.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1600","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1600&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/sheath-fold-eye-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.433548,58.550813]}},{"type":"Feature","properties":{"id":1586,"name":"Refolded isoclinal fold","description":"<p>Refolded isoclinal fold in Dalradian schists, Kinlochleven.<\/p>\n<p>Photograph: Tim Ivanic<\/p>\n","modified":"2018-06-30T13:03:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Refolded-isoclinal-fold-1-768x1024.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1586","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1586&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/refolded-isoclinal-fold-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.99929428101,56.71958015055486]}},{"type":"Feature","properties":{"id":1582,"name":"Portoro shear zone","description":"<p>Bedding-parallel Low Temperature (c.250 \u00b0C) shear zones observable in the Portoro limestone (Tuscan Nappe)<\/p>\n<p>Carter, K.E., 1992. 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Journal of Structural Geology (2010), doi: 10.1016\/ j.jsg.2010.11.015<\/p>\n<p>PhotoID346<\/p>\n<p>Photograph: G.Molli<\/p>\n","modified":"2018-07-24T11:10:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Portoro-shear-zone-202x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1582","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1582&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/portoro-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.846460309448233,44.03404113601831]}},{"type":"Feature","properties":{"id":1576,"name":"Slickenslide fault plane","description":"<p>A slickenside fault plane in a cataclasite. It is exposed in the core zone of the NASZ, defining the border between the Carboniferous Ploun\u00e9our-M\u00e9nez granite in the south and the Silurian-devonian Plougastel Formation in the north.<br \/>\nPhotoID342<\/p>\n<p>Photograph: Isaac Berwouts<\/p>\n","modified":"2018-09-04T11:45:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Slickenslide-fault-plane-768x583.jpg","taxonomy":{"webmapp_category":[220,230,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1576","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1576&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/slickenslide-fault-plane\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-3.82992625237,48.49632099933981]}},{"type":"Feature","properties":{"id":1574,"name":"Swan fold","description":"<p>Migmatitic garnet-biotite gneiss in the east-central portion of the Zona Transversal Domain Borborema Province in northeastern of Brazil. 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The character of disharmonic folds generated in the second stage is coupled to irregular granitic garnet-leucosome and provides a curious swan-shape, as shown in the image.<br \/>\nPhotoID341<\/p>\n<p>Photograph: Alan Miranda<\/p>\n","modified":"2018-06-28T14:53:46","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Swan-fold-768x544.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1574","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1574&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/swan-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-36.152497,-7.571612]}},{"type":"Feature","properties":{"id":1572,"name":"Antiformal stack","description":"<p>Antiformal stack of 3 folds (remp-flat system) at the beginning of Cimoliana Valley, Cimolais – Italy<br \/>\nPhotoID668<\/p>\n<p>Photograph:<\/p>\n<p>Reference: Geological map of Friuli region<\/p>\n","modified":"2018-06-30T11:17:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Antiformal-stack-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1572","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1572&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/antiformal-stack\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[12.474889755249023,46.3439651268241]}},{"type":"Feature","properties":{"id":1568,"name":"tonalite-monzogranite intrusion","description":"<p>Neoarchean (ca. 2680 Ma) granites displaying a well-defined planar fabric due to the injection of tonalite to monzogranite sheets aligned parallel to the magmatic foliation, which is defined by aligned euhedral feldspars. No effect of important solid-state deformation is visible at outcrop-scale. The base of photo is about 1 meter.<br \/>\nPhotoID339<\/p>\n<p>Photograph: Ivan Zibra<\/p>\n<p>Reference: Geological Survey of Western Australia (GSWA)<\/p>\n","modified":"2018-09-04T13:34:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/tonalite-monzogranite-intrusion-768x1024.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1568","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1568&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/tonalite-monzogranite-intrusion\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[117.50710487365723,-27.8917167699]}},{"type":"Feature","properties":{"id":1566,"name":"Layered intrusion","description":"<p>Layered kakortokites, Kangerdluarsuk, Ilimaussaq intrusion<br \/>\nPhotoID338<\/p>\n<p>Photograph: Tim Ivanic<\/p>\n","modified":"2018-06-30T11:35:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Layered-intrusion-768x576.jpg","taxonomy":{"webmapp_category":[232,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1566","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1566&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/layered-intrusion\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-45.8500671387,60.87099222956163]}},{"type":"Feature","properties":{"id":1775,"name":"Bertibubba Gneiss","description":"<p>Bertibubba Supersuite (c. 1965-1945 Ma; older name Wooramel Suite). Leucocratic augengneiss with strong subvertical EW planar fabric, gently E-plunging stretching lineation and good dextral shear sense indicators on horizontal surfaces. Dominant D1, the first phase of the Errabiddy shear zone deformation, related to the Glenburg Orogeny. The gneiss is supposed to be derived from partial melting of rocks like those of the Dalgaringa supersuite.<br \/>\nPhotoID473<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:52:47","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bertibubba-Gneiss-768x503.jpg","taxonomy":{"webmapp_category":[232,230,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1775","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1775&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/bertibubba-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.575333,-25.609167]}},{"type":"Feature","properties":{"id":1773,"name":"Yarweelor Gneiss","description":"<p>Yarweelor Gneiss (reworked Yilgarn gneiss – protolith 3.7-2.4 Ga). Gneissic layering (trending NS) is cut by an EW foliation associated with folds. The layering is probably an older Narryer direction and the folds are formed during D1-D2 in the Erabiddy shear zone.<br \/>\nPhotoID472<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:46:25","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Yarweelor-Gneiss-768x500.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1773","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1773&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/yarweelor-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.793833,-25.542833]}},{"type":"Feature","properties":{"id":1564,"name":"Cyclic igneous layering","description":"<p>The Windimurra vanadium pit, Windimurra Igneous Complex (c. 2810 Ma). Cyclic igneous layering of vanadiferous magnetitite, leucogabbro and anorthosite on a 1-5 metre scale can be seen here dipping to the west.<br \/>\nPhotoID337<\/p>\n<p>Photograph: Tim Ivanic<\/p>\n<p>Reference: Ivanic, T. J. , Wingate, M. T. D. , Kirkland, C. L. , Van Kranendonk, M. J. and Wyche, S.(2010).Age and significance of voluminous mafic-ultramafic magmatic events in the Murchison Domain, Yilgarn Craton, Australian. Journal of Earth Sciences, 57: 5, 597 \u2014 614<\/p>\n","modified":"2018-07-30T16:31:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cyclic-igneous-layering-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1564","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1564&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/cyclic-igneous-layering\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[118.53080749511719,-28.2921756112]}},{"type":"Feature","properties":{"id":1560,"name":"Box fold","description":"<p>Box fold. Northcott Mouth, North of Bude, Devon, England<br \/>\nPhotoID336<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T18:12:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Box-fold-768x503.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1560","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1560&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/box-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.555493,50.848006]}},{"type":"Feature","properties":{"id":1558,"name":"Mitre fold","description":"<p>Tight fold, known as Mitre fold. Belleville, New Brunswick, Canada<br \/>PhotoID334<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-15T10:22:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mitre-fold-199x300.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1558","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1558&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mitre-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-67.704628,46.203814]}},{"type":"Feature","properties":{"id":1556,"name":"Kink folds","description":"<p>Kink Folds in Carboniferous Culm facies. Hartland Quay, Devon, England<br \/>\nPhotoID333<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-07-30T16:29:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kink-folds-1-768x499.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1556","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1556&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/kink-folds-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.531395,50.995643]}},{"type":"Feature","properties":{"id":1554,"name":"Kink folds","description":"<p>Kink folded crenulation cleavage. Any planar structure will fold. Narooma, New South Wales, Australia.<br \/>\nPhotoID332<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T18:06:51","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kink-folds-768x514.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1554","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1554&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/kink-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[150.141292,-36.220436]}},{"type":"Feature","properties":{"id":1552,"name":"Ptygmatic folds","description":"<p>Linear ptygmatic folded quartz veins. Weekeroo, South Australia.<br \/>\nPhotoID331<\/p>\n<p>Photograph: Jim Talbot<\/p>\n<p>Reference: Other photos of folds with enveloping surfaces may be seen at: http:\/\/myweb.facstaff.wwu.edu\/talbot\/cdgeol\/Structure\/Fold\/Folds1\/Fold_styles.html#ptygmatic<\/p>\n","modified":"2018-06-30T11:14:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Ptygmatic-folds-768x497.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1552","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1552&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/ptygmatic-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[140.07076,-32.19229]}},{"type":"Feature","properties":{"id":1540,"name":"Red Dome fold","description":"<p>Red dome, an open fold. Red Dome, Bridger, MT. PhotoID324<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-30T19:33:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Red-Dome-fold-768x506.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1540","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1540&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/red-dome-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-108.856373,45.314084]}},{"type":"Feature","properties":{"id":1538,"name":"Unconformity","description":"<p>Permian sandstone on steeper dipping Silurian sandstone.<br \/>\nRichardson Mountains, Northwest Territories, Canada<br \/>\nPhotoID323<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T14:36:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Unconformity-1-768x503.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1538","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1538&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/unconformity-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-136.915284,67.993579]}},{"type":"Feature","properties":{"id":1771,"name":"Deformed conglomerate","description":"<p>Mt James formation conglomerate of facetted quartzite pebbles in a schist matrix; the Formation is dated at ca. 1800Ma. North is at the top<br \/>\nPhotoID471<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T12:46:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Deformed-conglomerate-1-768x502.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1771","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1771&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/deformed-conglomerate-4\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[115.969591,-25.152245]}},{"type":"Feature","properties":{"id":1769,"name":"Unconformity","description":"<p>Contact of the Mt James Formation and underlying metapelites of the Moogie Metamorphics. The Mt James Formation consists here of conglomerate with facetted quartzite pebbles in a schist matrix; the Formation is dated at ca. 1800Ma.<br \/>\nPhotoID470<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T16:15:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Unconformity-3-196x300.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1769","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1769&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/unconformity-4\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[115.960501,-25.15368]}},{"type":"Feature","properties":{"id":1536,"name":"Rip-up clasts","description":"<p>A 50cm thick bed with rip-up clasts in Silurian turbidites. Cliffs north of the river at Aberath, Wales.<br \/>\nPhotoID322<\/p>\n<p>Photograph: Jim Talbot<\/p>\n<p>Reference: Bates, D.E.B. 1982. The Aberystwyth Grits. p. 81-90, in Bassett, M.G. Geological Excursions in Dyfed, South West Wales. Geol Assoc, S Wales Group by the Nat Mus of Wales.<\/p>\n","modified":"2018-06-30T11:31:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rip-up-clasts-768x508.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1536","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1536&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/rip-up-clasts\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.221092,52.257747]}},{"type":"Feature","properties":{"id":1534,"name":"Big Penn slate quarry","description":"<p>Asymmetric anticline in Big Penn slate quarry. Slatedale, PA.<br \/>\nThe slate is mined by cutting it with cables and carborundum (the curved lines). The slate is then polished on rotating tables, again using carborundum as the abrasive. The best pieces are used for pool tables, but most is now used for ornamental paving.<br \/>\nPhotoID321<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T14:37:15","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Big-Penn-slate-quarry-768x503.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1534","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1534&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/big-penn-slate-quarry\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-75.660408,40.749519]}},{"type":"Feature","properties":{"id":1532,"name":"Fault line scarp","description":"<p>Mt Goodenough and the Mackenzie River delta, NWT, Canada. Mt Goodenough is part of an uplift hanging wall block.<br \/>\nPhotoID320<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T18:16:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fault-line-scarp-768x501.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1532","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1532&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/fault-line-scarp\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-135.445862,67.940206]}},{"type":"Feature","properties":{"id":1767,"name":"Deformed conglomerate","description":"<p>Mt James formation conglomerate of facetted quartzite pebbles in a schist matrix; the Formation is dated at ca. 1800Ma. North is at the top<br \/>\nPhotoID469<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:56:33","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Deformed-conglomerate-768x502.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1767","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1767&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/deformed-conglomerate-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[115.973354,-25.153833]}},{"type":"Feature","properties":{"id":1765,"name":"Unconformity","description":"<p>Contact of quartzite (white) of the Moogie metamorphics and conglomerate of the Mount James formation (centre). This is a ca. 1800 Ma old unconformity. Both formations are deformed by the Capricorn Orogeny, producing a vertical foliation<br \/>\nPhotoID468<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-10-23T13:53:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Unconformity-2-300x210.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1765","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1765&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/unconformity-3\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[115.966077,-25.155181]}},{"type":"Feature","properties":{"id":1530,"name":"Folded radiolarites in Corsica","description":"<p>At the pass of San Colombano, in the nappe of Balagne, thin, folded levels of red radiolarite and white quarzite lie on pillows lavas. The folds reversed towards the West are contemporaneous of the thrusting of alpine corsica on the hercynian basement. PhotoID315<\/p>\n<p>Photograph: c.nicollet<\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/Corse\/balagne\/balagne.html<\/p>\n","modified":"2019-05-16T12:24:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-radiolarites-in-Corsica-768x535.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1530","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1530&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/folded-radiolarites-in-corsica\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.077174663543701,42.579551093890814]}},{"type":"Feature","properties":{"id":1528,"name":"Dolerite sills","description":"<p>Intrusion of Ferrar dolerite sills in Beacon sandstone. Trio Nunatak, Victoria Land, Antarctica<br \/>\nPhotoID314<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p> <\/p>\n","modified":"2018-09-04T11:45:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Dolerite-sills-300x225.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1528","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1528&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/dolerite-sills\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[159.8123,-75.5156]}},{"type":"Feature","properties":{"id":1526,"name":"Shear zones","description":"<p>Shear zones with a top-to-the NE sense of shear affecting granites (light color) of the Granite Harbour Intrusives and amphibolite-facies metasediments (darks rocks) of the Wilson Metamorphics. Caudal Hills, Northern Victoria Land, Ross Orogen (Antarctica)<br \/>\nPhotoID313<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p>Reference: Meccheri, et al., Antarctic Geological 1:250.000 Map Series \u2013 Sequence Hills Quadrangle (Victoria Land), GIGAMAP, MURST-PNRA, in press.<\/p>\n","modified":"2018-06-30T12:37:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-zones-300x184.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1526","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1526&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/shear-zones\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[161.8622,-73.125]}},{"type":"Feature","properties":{"id":1763,"name":"shear band","description":"<p>shear band in mylonite of the Glenburg Orogeny. The mylonitites have gently W plunging lineation, and top-to-the-west shear sense. enlargement of the block below the hammer in 994307<br \/>\nPhotoID467<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:47:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/shear-band-768x497.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1763","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1763&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/shear-band\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.002901,-25.106554]}},{"type":"Feature","properties":{"id":1761,"name":"Glenburg orogeny mylonites","description":"<p>Halfway gneiss with gently W-dipping mylonitic foliation, looking North. There is a horizontal stretching lineation on the blocks in the foreground. At the back, the mapping case on the outcrop indicates the orientation of the foliation; here it is dipping steeply North. In fact, the outcrop shows a km-scale fold with gently W plunging axis (parallel to the stretching lineation) and vertical limbs.<br \/>\nIt is unlikely that this is the original geometry of the mylonite, so we deal with a gently dipping mylonite zone (thrust?? extensional decollement??) which was folded in NS shortening. The mylonite is cut by intrusions that belong to the Dalgaringa supersuite, and is therefore older than 1970Ma, and belongs to deformation in the Glenburg orogeny, not the Capricorn orogeny; the folding may be of Capricorn orogeny age<br \/>\nPhotoID466<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:38:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Glenburg-orogeny-mylonites-768x500.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1761","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1761&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/glenburg-orogeny-mylonites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[116.00306193254096,-25.1063791267]}},{"type":"Feature","properties":{"id":1751,"name":"Gran Cono","description":"<p>alternation of lava flows and pyroclastic deposits<br \/>\nPhotoID461<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-30T12:07:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Gran-Cono-1-763x1024.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1751","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1751&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/gran-cono-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.427881240844727,40.81881095338081]}},{"type":"Feature","properties":{"id":1745,"name":"Boudinage","description":"<p>Buodinage in Liassic Marbles.<br \/>Seravezza, Alpi Apuane.<br \/>PhotoID456<\/p>\n<p>Photograph: F.Milazzo<\/p>\n<p>Reference: I MARMI DELLE ALPI APUANE (TOSCANA SETTENTRIONALE) Carmignani L., Conti P., Fantozzi P., Mancini S. , Massa G, Molli G., Vaselli L.; GEOLOGY OF THE ALPI APUANE METAMORPHIC COMPLEX (ALPI APUANE, CENTRAL ITALY) AUTHORS: L. Carmignani, P. Conti, M. Meccheri, G. Molli, Volume n\u00b0 5 – from P37 to P54; LINEAMENTI GEOLOGICI DELLE ALPI APUANE Luigi Carmignani, Paolo Conti, Giovanni Massa, Luca Vaselli, Sergio Mancini Acta Apuana, Suppl. V (2006), 9-23<\/p>\n","modified":"2018-06-15T10:22:07","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Boudinage-768x1024.jpg","taxonomy":{"webmapp_category":[228]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1745","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1745&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/boudinage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.230444073677063,43.98874472203971]}},{"type":"Feature","properties":{"id":1524,"name":"Pillows lavas of the Monte Viso","description":"<p>Monte Viso is a portion of the ligurian oceanic crust subducted at more than 2 GPa. At the bottom of the mountain, blue pillows lavas are<br \/>\nundeformed.The blue color is due to fine needles of glaucophane. PhotoID307<\/p>\n<p>Photograph: c.nicollet<\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/Viso\/viso.html<\/p>\n","modified":"2018-07-24T12:28:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pillows-lavas-of-the-Monte-Viso-768x576.jpg","taxonomy":{"webmapp_category":[232,234,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1524","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1524&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/pillows-lavas-of-the-monte-viso\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.115278244018555,44.66346411852218]}},{"type":"Feature","properties":{"id":1935,"name":"synvolcanic faulting in BIF","description":"<p>Small-scale faults at high-angle from the primary bedding in the c. 2.8 Ga banded iron formation near Mount Magnet. The gap created during faulting is filled by basaltic lava flows. Photo ID 670<\/p>\n<p>Photograph: ivan zibra<\/p>\n<p>Reference: Geological Survey of Western Australia. http:\/\/www.dmp.wa.gov.au\/371.aspx<\/p>\n","modified":"2018-06-15T10:22:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/synvolcanic-faulting-in-BIF-768x575.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1935","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1935&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/synvolcanic-faulting-in-bif\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[117.80030250549316,-28.0561130003]}},{"type":"Feature","properties":{"id":1743,"name":"Rheomorfic folds","description":"<p>Reomorfic folds in Komenditic lava flows (peralkalyne rhiolyte). From San Pietro island, SW Sardinia.<br \/>\nPhotoID455<\/p>\n<p>Photograph: D. Pieruccioni<\/p>\n<p>Reference: Cioni R., Funedda A. (2005): Structural geology of crystal-rich, silicic lava flows: A case study From San Pietro Island (Sardinia, Italy).Geological Society or America Special Paper 396; Cioni R., Salaro L., Pioli L. (2001): The Cenozoic volcanism of San Pietro Island (Sardinia, Italy). Rendiconti Seminario Facolt\u00e0 Scienze Universit\u00e0 Cagliari Supplemento Vol. 71 Fasc. 2<\/p>\n","modified":"2018-06-28T13:37:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Rheomorfic-folds-768x576.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1743","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1743&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/rheomorfic-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.226571083068848,39.15644601929688]}},{"type":"Feature","properties":{"id":1741,"name":"refolded D1 structure","description":"<p>Interference of mesoscale folds: the first-phase structures<br \/>\ndeform the contact between the Rhetic Chloritoid Schists and Breccia of Seravezza.<br \/>\nPhotoID453<br \/>\nThe contact is characterized by isoclinal folds anticlines and synclines that shows a M geometry.<br \/>\nThe first deformation event (D1) is related to the phase of underthrusting of the tectonics units.<br \/>\nThe second deformation event refolds the previous structures (D2) and gives rise to open folds with sub-horizontal axial plane foliation.<br \/>\nD2 deformation event is related to the exhumation of the the Alpi Apuane metamorphic complex.<\/p>\n<p>Photograph: F.Milazzo<\/p>\n<p>Reference: Franceschelli M. , Puxeddu M. ,Carcangiu G. ,Gattiglio M. ,Pannuti F. (1996) \u2013 Breccia-hosted manganese-rich minerals of Alpi Apuane, Italy : A marine, redoxgenerated deposits; Franceschelli M. , Puxeddu M. , Memmi I. (1998) – Li, B-rich Rhaetian metabauxite, Tuscany, Italy : reworking of older bauxites and igneous rocks Chemical Geology 144, 221-242; Franceschelli M. & Memmi I. (1999) \u2013 Zoning of chloritoid from kyanite-facies metapsammites, Alpi Apuane, Italy, Mineralogical Magazine, 63, 105-110; Franceschelli M. , Puxeddu M. ,Gattiglio M. (2003) – Geochemistry and origin of chloritoid schist from the Alpi Apuane, Italy: evidence of a prevailing lateritic signature Eur. J. Mineral. 15, 575-588.<\/p>\n","modified":"2019-02-02T07:23:52","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/refolded-D1-structure-1-768x575.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1741","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1741&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/refolded-d1-structure-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.292526483535767,44.03723392161239]}},{"type":"Feature","properties":{"id":1522,"name":"Superposed folds in marbles","description":"<p>Superposed folds in the Santa Catalina marbles ; east coast of the Alpine Corsica. On the right photography, the axes of the 2 generations of the folds are perpendicular ; they are parallel on the left photography.<br \/>\nPhotoID297<\/p>\n<p>Photograph: ch.nicollet<\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/Corse\/CapCorse\/CoteE.html<\/p>\n","modified":"2018-06-28T18:10:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Superposed-folds-in-marbles-768x353.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1522","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1522&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/superposed-folds-in-marbles\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.486383199691772,42.82344849130125]}},{"type":"Feature","properties":{"id":1520,"name":"Half graben of Lac Besson","description":"<p>Many hectometric half-grabens of the margin of the alpine ocean are visible near the Lac Besson.<br \/>\nUnder the foot of Mireille, the escarpment of the normal fault consists of hercynian gneisses. The half graben is filled with red triassic dolomites which rest unconformably on the Hercynian basement on the right side of the photography (to the East). PhotoID296<\/p>\n<p>Photograph: ch.nicollet<\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/ornon\/besson.html<\/p>\n","modified":"2018-06-30T11:07:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Half-graben-of-Lac-Besson-768x288.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1520","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1520&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/half-graben-of-lac-besson\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.089880466461182,45.121665339526665]}},{"type":"Feature","properties":{"id":1739,"name":"Turbidite deposits","description":"<p>The Turbidite deposits of the photo (Flysch of Solignano Fm.) consist of Maastrichtian alternations of sandstones and mudstones interbedded with marly limestones and silty marls.<br \/>\nThe Flysh of Solignano belongs to the Solignano Units (Ligure Domain )<br \/>\nPhotoID452<\/p>\n<p>Photograph: F.Milazzo<\/p>\n<p>Reference: 1983 D. Rio & Villa G – I nannofossili calcarei del Cretacico superiore del Flysch di Solignano, media Val Taro – Appennino Settentrionale. Mem. Soc Geol. Padova , 36, 239-282; G. PLESI , L. BIANCHI , S. CHICCHI & G. DANIELE THE LIGURIAN AND EMILIAN UNITS OF THE MIDDLE TARO VALLEY (NORTHERN APENNINES) AND THEIR STRUCTURAL EVOLUTION Atti Tic. Sc. Terra 36 (1993), 183-229; C1 – FONTANA D., STEFANI C., ZUFFA G.G. e TATEO F., 1990, Il Flysch di Solignano nel quadro dei Flysch ad Elmintoidi (Maastrichtiano inferiore, Appennino settentrionale: Giornale di Geologia, v. 52\/1-2, p.99-120. ZANZUCCHI G. (1967) – Osservazioni preliminari sulla tettonica della media Val di Taro (Carta Geologica 1:50.000 e sezioni). Ateneo Parmense, Acta Nat., 3: 59-89, Parma [8].<\/p>\n","modified":"2018-06-30T11:23:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Turbidite-deposits-768x575.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1739","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1739&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/turbidite-deposits\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.987441301345825,44.61615065409093]}},{"type":"Feature","properties":{"id":1737,"name":"Col Ombert and diapiric anticline","description":"<p>Permian Bellerophon FM forming a diapiric antickline plus Col Ombert thrsts – San Nicol\u00f2 Valley – Dolomites<br \/>\nView from Magnifici 4 Via ferrata<br \/>\nPhotoID669<\/p>\n<p>Photograph: Max Scarpa<\/p>\n<p>Reference: – Bosellini A. Geology of Dolomites AA. VV. 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(1996) \u2013 Breccia-hosted manganese-rich minerals of Alpi Apuane, Italy : A marine, redoxgenerated deposits; Franceschelli M. , Puxeddu M. , Memmi I. (1998) – Li, B-rich Rhaetian metabauxite, Tuscany, Italy : reworking of older bauxites and igneous rocks Chemical Geology 144, 221-242; Franceschelli M. & Memmi I. (1999) \u2013 Zoning of chloritoid from kyanite-facies metapsammites, Alpi Apuane, Italy, Mineralogical Magazine, 63, 105-110; Franceschelli M. , Puxeddu M. ,Gattiglio M. (2003) – Geochemistry and origin of chloritoid schist from the Alpi Apuane, Italy: evidence of a prevailing lateritic signature Eur. J. Mineral. 15, 575-588<\/p>\n","modified":"2018-09-04T11:44:17","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/refolded-D1-structure-617x1024.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1733","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1733&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/refolded-d1-structure\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.292569398880005,44.03759642369555]}},{"type":"Feature","properties":{"id":1731,"name":"Fault Plane","description":"<p>Fault plane with cataclasite in Liassic marbles. Pania della Croce, Alpi Apuane<br \/>\nPhotoID445<\/p>\n<p>Photograph: F.Milazzo<\/p>\n<p>Reference: Maxwell J. C. ,(1956) \u2013 Tectonics of Pania della Croce \u2013 Pania Secca area, Alpi; Apuane Bol. Soc. Geol. It. , 75 (2), 57-78 Mem. Soc. Geol. It., 28, 549-576. Raffaello Nardi, GEOLOGIA DELLA ZONA TRA LA PANIA DELLA CROCE, GALLICANO E CASTELNUOVO GARFAGNANA (ALPI APUANE). 1961<\/p>\n","modified":"2018-10-23T13:53:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fault-Plane-768x1024.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1731","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1731&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/fault-plane\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.32154530286789,44.03834263110903]}},{"type":"Feature","properties":{"id":1729,"name":"Folded and boudinaged gabbroic pegmatite","description":"<p>Folded and boudinaged gabbroic pegmatite intruded into host two-<br \/>Px gabbro. The vein outline is detectable by the higher plagioclase content and by the coarser grain size. Some hornblende porphyroclasts occur along the upper sheared limb.<br \/>PhotoID444<\/p>\n<p>Photograph: Ivan Zibra<\/p>\n<p>Reference: Reference: Zibra I, Kruhl JH, Braga R (2010). Late Palaeozoic deformation of post-Variscan lower crust: shear zone widening due to strain localization during retrograde shearing. Int J Earth Sci (Geol Rundsch) DOI 10.1007\/s00531-009-0441-5<\/p>\n","modified":"2018-06-15T10:21:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folded-and-boudinaged-gabbroic-pegmatite-768x576.jpg","taxonomy":{"webmapp_category":[228]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1729","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1729&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/folded-and-boudinaged-gabbroic-pegmatite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.221241474151611,42.30461040225633]}},{"type":"Feature","properties":{"id":1518,"name":"Mini graben of Gandaillat","description":"<p>The mini graben of Gandaillat is a reduced version of the rift of Limagne<br \/>PhotoID287<\/p>\n<p>Photograph: <\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/Figures\/Limagne\/Limagne.html<\/p>\n","modified":"2018-06-15T10:21:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mini-graben-of-Gandaillat-768x501.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1518","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1518&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mini-graben-of-gandaillat\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.154771327972412,45.773420143839864]}},{"type":"Feature","properties":{"id":1504,"name":"Ecum Secum","description":"<p>Folded crossbedded sandstone in slate, Ecu Secum. 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Lyon I<\/p>\n","modified":"2018-09-16T10:30:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Leptyno-amphibolitic-group-225x300.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1502","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1502&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/leptyno-amphibolitic-group\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.75931,45.06425]}},{"type":"Feature","properties":{"id":1472,"name":"Ripple Marks, Quarziti Fm.","description":"<p>Ripple Marks in quartzite.<br \/>\nQuarziti Monte Serra Fm.<br \/>\nQuarziti Viola-Zonate Mb.<br \/>\nPhotoID255<\/p>\n<p>Photograph: S. Papeschi<\/p>\n<p>Reference: RAU A., TONGIORGI M. (1974) – Geologia dei Monti Pisani a Sud-Est della valle del Guappero<\/p>\n","modified":"2018-06-28T14:52:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Ripple-Marks-Quarziti-Fm-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1472","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1472&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/ripple-marks-quarziti-fm\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.490983128547668,43.743072685069606]}},{"type":"Feature","properties":{"id":1470,"name":"Turbidite sequence, Macigno fm.","description":"<p>Turbidite showing a fining upward succession.<br \/>\nWe can recognize 2 beds of the Bouma Sequence.<br \/>\nStarting from the bottom:<\/p>\n<p>A – Granules and very coarse sand (Gravelly Sandstone to Lithic Sandstone)<br \/>\nB – Parallel laminated sandstone.<br \/>\nPhotoID254<\/p>\n<p>Photograph: S. Papeschi<\/p>\n<p>Reference: none.<\/p>\n","modified":"2018-06-28T14:48:59","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Turbidite-sequence-Macigno-fm-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1470","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1470&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/turbidite-sequence-macigno-fm\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.35135269165039,43.463634904411194]}},{"type":"Feature","properties":{"id":1460,"name":"Arkitsa Fault","description":"<p>Segment of the Arkitsa Fault zone with corrugations and open tension fractures on the exposed fault surface.<br \/>\nPhotoID250<\/p>\n<p>Photograph: Sotiris Kokkalas<\/p>\n<p>Reference: Jones et al. (2009) Geosphere v.5, n.6, p. 1-18<\/p>\n","modified":"2018-06-28T14:57:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Arkitsa-Fault-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1460","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1460&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/arkitsa-fault-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[23.00662636756897,38.732410041502824]}},{"type":"Feature","properties":{"id":1458,"name":"Abandoned quarry, Quarziti Fm.","description":"<p>Ichnofacies, ripple marks<br \/>\nPhotoID248<\/p>\n<p>Photograph: S. Papeschi<\/p>\n<p>Reference: RAU A., TONGIORGI M. (1974) – Geologia dei Monti Pisani a Sud-Est della valle del Guappero<\/p>\n","modified":"2018-06-30T11:26:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Abandoned-quarry-Quarziti-Fm-768x1024.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1458","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1458&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/abandoned-quarry-quarziti-fm\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.49117624759674,43.743072685069706]}},{"type":"Feature","properties":{"id":1456,"name":"Ripple marks, Scisti Verdi Fm","description":"<p>Ripple Marks in association with sole marks of halite crystals and mudcracks.<br \/>\nMt. Terminetto, Pisa<br \/>\nPhotoID247<\/p>\n<p>Photograph: S. Papeschi<\/p>\n<p>Reference: RAU A., TONGIORGI M. 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Type 3 interference pattern (Ramsay, 1967).<br \/>Varicolured Sericitic Schists of the epimetamoprhic Tuscan succession (tectonic complex n. 3) at Cala dell\u2019Alga, Elba Island (Italy).<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p>Reference: Benvenuti et al. (2001) \u2013 B Eastern Elba (field trip). Ofioliti, 26 (2a), 331-346.<\/p>\n","modified":"2018-06-15T10:21:14","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Refolded-folds-768x516.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1422","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1422&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/refolded-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.421267,42.865852]}},{"type":"Feature","properties":{"id":1420,"name":"Overturned pillow lavas","description":"<p>Overturned pillow lavas in the Ligurid Units of Elba island (tectonic complex n. 4). 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Carosi<\/p>\n","modified":"2018-06-30T12:27:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Overturned-pillow-lavas-768x516.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1420","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1420&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/overturned-pillow-lavas\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.202813,42.806814]}},{"type":"Feature","properties":{"id":1418,"name":"Magmatic foliation in a granodiorite","description":"<p>Magmatic foliation in the Mt. Capanne granodiorite (c. 7 Ma) marked by the preferred orientation of cm-size feldspars . Punta S. Andrea, Elba island (italy).<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p>Reference: Dini et al. (2002) – Geological Magazine, 139, 257-279.<\/p>\n","modified":"2018-06-30T19:14:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Magmatic-foliation-in-a-granodiorite-768x516.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1418","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1418&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/magmatic-foliation-in-a-granodiorite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.140329,42.808823]}},{"type":"Feature","properties":{"id":1411,"name":"Rotated boudin, Dry Valleys","description":"<p>Roatated boudin in high-grade marbles deformed during the Ross Orogen (Nussbaum Riegel, Taylor Valley, Victoria Land; Antarctica)<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p> <\/p>\n","modified":"2019-02-23T08:51:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Asymmetric-boudins-Dry-Valleys-e1530184771899-768x576.jpg","taxonomy":{"webmapp_category":[228]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1411","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1411&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/rotated-boudin-dry-valleys\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[161.446969,-77.39112]}},{"type":"Feature","properties":{"id":1409,"name":"Flanking folds and boudins","description":"<p>This photograph shows modified boudin structures from Wilson Bluff in the Southern Prince Charles Mountains, East Antarctica. There is an impressive flanking-fold structure situated between the torn mafic boudins, that presumably formed by ductile flow of the overlying host grey gneiss into a low-pressure sink during the boudin separation. Subsequent reworking and shortening is indicated by numerous folded boudin structures in the leucocratic pegmatite material. The timing of the structures is uncertain but the host rock is of Precambrian age. The exposure is southwest facing. PhotoID200<\/p>\n<p>Photograph: Adrian F Corvino<\/p>\n<p>Reference: This is a photograph of the Month in the Journal of Structural geology (JSG 32, 1)<\/p>\n","modified":"2018-06-15T10:21:02","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Flanking-folds-and-boudins-768x509.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1409","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1409&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/flanking-folds-and-boudins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[66.78333,-70.3]}},{"type":"Feature","properties":{"id":1399,"name":"Tudela leucosomes","description":"<p>Leucosome pods in migmatitic schists from Tudela (former ClubMed) in the Cap de Creus tectonometamorphic belt. Notice the complex folding around the pods. PhotoID197<\/p>\n<p>Photograph: Elena Druguet<\/p>\n<p>Reference: Druguet, E., Carreras, J. 2006. Analogue modelling of syntectonic leucosomes in migmatitic schists. Journal of Structural Geology 28, 1734-1747.<\/p>\n","modified":"2018-09-04T15:56:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Tudela-leucosomes-768x576.jpg","taxonomy":{"webmapp_category":[229,234]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1399","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1399&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/tudela-leucosomes\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.294842317700386,42.3270494869462]}},{"type":"Feature","properties":{"id":1397,"name":"Shear zone Mt. 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Metamorphic Geology, 5, 605-630.<\/p>\n","modified":"2018-06-28T18:10:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Shear-zone-Mt.-Emison-768x516.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1397","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1397&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/shear-zone-mt-emison\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[163.936938,-74.21443]}},{"type":"Feature","properties":{"id":1393,"name":"F1 fold, Scaglia Toscana","description":"<p>Urpight F1 folds in pelites and limestones of the Scaglia Toscana Formation and refraction of S1 continuos foliation. 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View south of Great Slave Lake, Yellowknife, Northwest Territories, Canada. The fault displaces the Giant Yellowknife ore body from the mine on the light colored peninsular on the left to the mine complex near the top of the photo to the right of the fault. This makes it a left lateral fault.<br \/>\nPhotoID319<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-28T18:04:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/West-Bay-Fault-Yellowknife-768x503.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1514","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1514&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/west-bay-fault-yellowknife\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-114.368763,62.479704]}},{"type":"Feature","properties":{"id":1512,"name":"Penrhyn slate","description":"<p>Fence of Ordovician slate from the Penrhyn quarries. The light-coloured spots, up to five cm by two cm on the cleavage, and <1cm thick, were spherical spots in mud before the rocks deformed during the Caledonian collision.<br \/>PhotoID318<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-15T10:18:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Penrhyn-slate-200x300.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1512","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1512&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/penrhyn-slate\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.045215,53.158315]}},{"type":"Feature","properties":{"id":1510,"name":"South Stack, Anglesey","description":"<p>Lighthouse with large second generation folds in schist. 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Geodinamica Acta, 10, 94-114.<\/p>\n","modified":"2018-06-30T11:08:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-giant-porphyroclast-719x1024.jpg","taxonomy":{"webmapp_category":[232,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1508","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1508&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/a-giant-porphyroclast\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[44.905242919921875,-24.4908978153]}},{"type":"Feature","properties":{"id":1506,"name":"A normal fault, Malaga","description":"<p>A normal fault<br \/>PhotoID312<\/p>\n<p>Photograph: c.nicollet<\/p>\n","modified":"2018-06-15T10:18:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-normal-fault-Malaga-300x198.jpg","taxonomy":{"webmapp_category":[230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1506","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1506&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/a-normal-fault-malaga\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.37715053558,36.736141388028194]}},{"type":"Feature","properties":{"id":1500,"name":"Mt. 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Ophiolite Massif of Chenaillet<br \/>\nPhotoID310<\/p>\n<p>Photograph: c.nicollet<\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/chenaillet\/chenaillet.html<\/p>\n","modified":"2018-07-24T11:10:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/The-pillows-lavas-of-the-Collet-Vert-768x530.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1498","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1498&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/the-pillows-lavas-of-the-collet-vert\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.750755310055796,44.90974370958705]}},{"type":"Feature","properties":{"id":1496,"name":"The K\/T boundary in the Basque coast.","description":"<p>The Cretaceous-Tertiary boundary is well exposed on the beach of Bidart (4km south of Biarritz). A 20cm thick Iridium rich level of black shales separates the grey Maestrichian limestone (on the bottom) and the white Danian limestones (on the top). The K-T transition seems to be continuous. PhotoID309<\/p>\n<p>Photograph: c.nicollet<\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/limiteK-T\/KT.html<\/p>\n","modified":"2018-06-28T14:38:00","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/The-KT-boundary-in-the-Basque-coast-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1496","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1496&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/the-k-t-boundary-in-the-basque-coast\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-1.58585071564,43.450247382932425]}},{"type":"Feature","properties":{"id":1494,"name":"A reverse fault – Djebel Akhdar","description":"<p>A reverse fault in the Djebel Akhdar – Oman<\/p>\n<p>PhotoID308<\/p>\n<p>Photograph: c.nicollet<\/p>\n","modified":"2018-09-03T17:45:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-reverse-fault-Djebel-Akhdar-768x462.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1494","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1494&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/a-reverse-fault-djebel-akhdar\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[57.398441433906555,23.19427475983768]}},{"type":"Feature","properties":{"id":1492,"name":"A typical ligurian ophiolitic sequence","description":"<p>The alpine Chenaillet ophiolite is characteristic of an oceanic crust created at a low spreading ridge. The sequence is discontinuous and differs from the classical sequence of the Penrose conference.<br \/>\nFrom the bottom to the top of the SW ridge of the Chenaillet, we have the sequence : serpentinized mantle, isotropic gabbro and pillows lavas. The dyke complex is missing. Only a few dykes crosscut the serpentinite or the gabbro. Sometimes, the sediments directly lie on the serpentinized mantle.<br \/>\nView towards the NE from the Sommet des Anges.<br \/>\nPhotoID306<\/p>\n<p>Photograph: c.nicollet<\/p>\n<p>Reference: http:\/\/christian.nicollet.free.fr\/page\/Alpes\/chenaillet\/chenaillet.html<\/p>\n","modified":"2018-10-10T18:48:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/A-typical-ligurian-ophiolitic-sequence-768x512.jpg","taxonomy":{"webmapp_category":[234,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1492","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1492&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/a-typical-ligurian-ophiolitic-sequence\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.71565055847168,44.893214870201454]}},{"type":"Feature","properties":{"id":1490,"name":"Augen gneiss","description":"<p>Mylonitic augen gneiss with rotated porphyroclastst and C-S fabric (top-to-the<br \/>\nNW sense of shear) developed during a regional dextral shearing at nearly 320 Ma in the Variscan Basement of Sardinia<br \/>\nPhotoID305<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p>Reference: CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. Journal of the Virtual Explorer, Volume 22, Paper 3.<\/p>\n","modified":"2018-06-28T13:34:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Augen-gneiss-300x225.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1490","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1490&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/augen-gneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.563934,40.600243]}},{"type":"Feature","properties":{"id":1488,"name":"Cm-size staurolite","description":"<p>Cm-size Staurolite crystals in garnet+staurolite bearing micaschist partly reoriented on the S2 foliation. Variscan Basement of northern Sardinia.<br \/>\nPhotoID304<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p>Reference: CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. Journal of the Virtual Explorer, Volume 22, Paper 3.<\/p>\n","modified":"2018-06-30T12:58:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cm-size-staurolite-300x225.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1488","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1488&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/cm-size-staurolite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.582494,40.601903]}},{"type":"Feature","properties":{"id":1482,"name":"Mylonitic granodiorite","description":"<p>C-S fabric in granodioritic orthogneiss (top-to-the NW sense of shear) developed during a regional dextral shearing at nearly 320 Ma in the Variscan Basement of Sardinia.<br \/>\nPhotoID303<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p>Reference: CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. Journal of the Virtual Explorer, Volume 22, Paper 3.<\/p>\n","modified":"2018-07-24T12:22:54","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitic-granodiorite-300x203.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1482","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1482&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mylonitic-granodiorite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.592778,40.594556]}},{"type":"Feature","properties":{"id":1480,"name":"Coronitic eclogite of Sifah","description":"<p>The centimetric garnet of the eclogite is surrounded by a corona of glaucophane. It indicates a retrogression from the eclogite conditions to the blueschists conditions during the exhumation of the rock. Yellow epidote and dark blue glaucophane constitute the matrix of rock. PhotoID302<\/p>\n<p>Photograph: ch.nicollet<\/p>\n","modified":"2018-06-15T10:17:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Coronitic-eclogite-of-Sifah-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1480","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1480&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/coronitic-eclogite-of-sifah\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[58.7794303894043,23.454900281161684]}},{"type":"Feature","properties":{"id":1478,"name":"Zimudang thrust","description":"<p>Reversed anticline in the hangingwall of a thrust fault in Permian \u2013Triassic limestone. The cataclasite hosts gold and cinnabar deposits. Zimudang mine (Guizhou Province, China) PhotoID301<\/p>\n<p>Photograph: R. Carosi<\/p>\n<p>Reference: R. Carosi – Unipi<\/p>\n","modified":"2018-06-28T14:51:28","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Zimudang-thrust-300x203.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1478","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1478&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/zimudang-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[105.470596,25.572227]}},{"type":"Feature","properties":{"id":1476,"name":"Synsedimentary graben","description":"<p>Synsedimentary graben in the Miocene StFlorent basin. 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Photo on an horizontal surface (YZ plane); on a vertical plane the breccia is stretched, probably by the ca. 3.2 Ga deformation.<\/p>\n<p>Kisters, A.F.M., Anhaeusser, C.R., 1995. Emplacement features of Archaean TTG plutons along the Southern margin of the Barberton greenstone belt, South Africa. 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This one presents a high pressure blueschist-eclogite facies metamorphic rock. Notice the beautiful green due to the mineral omphacite (pyroxene group). Below this is a marble formation and ophiolithic melange.<br \/>\nPhotoID246<\/p>\n<p>Photograph: Exakoustidis Miltiadis, Athens<\/p>\n","modified":"2018-06-30T12:44:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Exotic-Slices-768x529.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1335","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1335&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/exotic-slices\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[24.935504,37.496545]}},{"type":"Feature","properties":{"id":1333,"name":"Cordilleran orogenic base","description":"<p>Thin vein (grey layer) of the 1.9 Ga Bourne granite suite crosscutting a fold train of orthogneiss and amphibolite layers. Located a few meters below the Cordilleran orogenic base mapped in the northern Monashee Complex of the southeastern Canadian Cordillera.<\/p>\n<p>Crowley, J.L., Brown, R.L., Gervais, F., Gibson, H.D. (2008). Assessing zircon and monazite inheritance in granitic rocks; an example from the Monashee Complex, Canadian Cordillera. Journal of Petrology 49, 1915-1929.<br \/>Gervais, F., Brown, R.L., Crowley, J.L. (2010). Tectonic implications for a Cordilleran orogenic base in the Frenchman Cap dome, southeastern Canadian Cordillera. Journal of Structural Geology 32, 941-959.<\/p>\n<p>PhotoID237<\/p>\n<p>Photograph: F\u00e9lix Gervais<\/p>\n","modified":"2018-06-15T10:16:38","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Cordilleran-orogenic-base-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1333","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1333&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/cordilleran-orogenic-base\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.588399887,51.3353977950284]}},{"type":"Feature","properties":{"id":1323,"name":"deformed dyke above orogenic base","description":"<p>Highly deformed 1.9 Ga Bourne granite dyke (grey layer) located ca. 1 km structurally above the Cordilleran orogenic base mapped in the northern Monashee Complex of the southeastern Canadian Cordillera.<\/p>\n<p>Crowley, J.L., Brown, R.L., Gervais, F., Gibson, H.D. (2008). Assessing zircon and monazite inheritance in granitic rocks; an example from the Monashee Complex, Canadian Cordillera. Journal of Petrology 49, 1915-1929.<br \/>\nGervais, F., Brown, R.L., Crowley, J.L. (2010). Tectonic implications for a Cordilleran orogenic base in the Frenchman Cap dome, southeastern Canadian Cordillera. Journal of Structural Geology 32, 941-959.<br \/>\nPhotoID236<\/p>\n<p>Photograph: F\u00e9lix Gervais<\/p>\n","modified":"2018-06-30T12:41:42","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/deformed-dyke-above-orogenic-base-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1323","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1323&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/deformed-dyke-above-orogenic-base\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.602240086,51.38483889332912]}},{"type":"Feature","properties":{"id":1321,"name":"melt-filled conjugate shear zones","description":"<p>Melt-filled, conjugate shear zones developed in granitic orthogneisses of the Grenville Province along the shore of the St-Lawrence River (Quebec). 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Gneiss domes in Orogeny: Geological Society of America Special Paper 380, p. 359-378.<\/p>\n<p>PhotoID235<\/p>\n<p>Photograph: F\u00e9lix Gervais<\/p>\n","modified":"2018-06-15T10:16:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/melt-filled-conjugate-shear-zones-768x510.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1321","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1321&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/melt-filled-conjugate-shear-zones\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-62.4802780151,50.26147330918773]}},{"type":"Feature","properties":{"id":1309,"name":"Nilgiril Anticline","description":"<p>View to the east across the Kali Gandaki from the trail leading toward Hidden Valley and Dhaulagiri basecamp to the Nilgiri Peaks (7061m, 6940m, 6839m respectively from north to south). 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Larson<\/p>\n","modified":"2018-06-28T18:13:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Nilgiril-Anticline-768x527.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1309","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1309&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/nilgiril-anticline\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.726806640625,28.66769613249295]}},{"type":"Feature","properties":{"id":1307,"name":"Refolded isoclinal fold","description":"<p>Isoclinal F1 synform refolded by F2 open folds (type 3 interference pattern) in white quartzites containing phengite, glaucophane and garnet. 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Carosi<\/p>\n","modified":"2018-06-15T10:16:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Refolded-isoclinal-fold-201x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1307","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1307&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/refolded-isoclinal-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.32627,42.50975]}},{"type":"Feature","properties":{"id":1297,"name":"sheath fold","description":"<p>Sheath fold, view in a section peprendicular to the stretching lineation, in white quartzites containing phengite, glaucophane and garnet. 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Carosi<\/p>\n","modified":"2018-06-28T14:46:03","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sheath-fold-300x201.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1297","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1297&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/sheath-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[9.32594,42.50907]}},{"type":"Feature","properties":{"id":1295,"name":"Mt. 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Carosi<\/p>\n","modified":"2018-07-25T08:46:09","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mt.-Makalu-south-face-768x516.jpg","taxonomy":{"webmapp_category":[234,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1295","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1295&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mt-makalu-south-face\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.076445,27.837501]}},{"type":"Feature","properties":{"id":1293,"name":"Arkitsa fault","description":"<p>One of the largest fresh fault surfaces in the world with very well preserved striations.<\/p>\n<p>Jackson J. & McKenzie D. (1999). DOI: 10.1016\/S0191-8141(98)00091-1<br \/>\nJones R.R. et al. (2009). DOI: 10.1130\/GES00216.1<br \/>\nResor P.G. & Meer V.E. (2009). DOI: 10.1016\/j.epsl.2009.10.010<\/p>\n<p>Photograph: Alex CHATZIPETROS<\/p>\n","modified":"2018-06-28T14:38:37","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Arkitsa-fault-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1293","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1293&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/arkitsa-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[23.00759732723236,38.732150592296996]}},{"type":"Feature","properties":{"id":1287,"name":"San Andreas folds and faults","description":"<p>Contractional deformation near Palmdale along the San Andreas fault zone, representing a complex hard-linked restraining stepover structure. Complexly folded and faulted rocks of the Anaverde Formation (lower to middle Pliocene) are unconformably overlain by Pleistocene sediments.<\/p>\n<p>Fife, D. L. & Minch, J. A. 1982. In: Geology and mineral wealth of the California Traverse Ranges. South Coast Geological Society, 78-93.<\/p>\n<p>http:\/\/strike-slip.geol.ucsb.edu\/KESSEL\/palmdaleroadcut.html<\/p>\n<p>Photograph: Haakon Fossen<\/p>\n","modified":"2018-06-28T18:13:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/San-Andreas-folds-and-faults-768x404.jpg","taxonomy":{"webmapp_category":[220,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1287","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1287&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/san-andreas-folds-and-faults\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-118.13379,34.563255]}},{"type":"Feature","properties":{"id":1285,"name":"Upright folds","description":"<p>Folds exposed by the parking lot next to the Calico ghost town near Barstow, CA. These folds appear to be related to local contraction along strike-slip faults in the area. <\/p>\n<p>Photograph: Haakon Fossen<\/p>\n","modified":"2018-06-15T10:16:22","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Upright-folds-1-768x395.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1285","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1285&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/upright-folds-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-116.865864,34.947162]}},{"type":"Feature","properties":{"id":1283,"name":"Upright folds","description":"<p>Folds exposed by the parking lot next to the Calico ghost town near Barstow, CA. These folds appear to be related to local contraction along strike-slip faults in the area. <\/p>\n<p>Photograph: Haakon Fossen<\/p>\n","modified":"2018-06-15T10:16:18","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Upright-folds-768x395.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1283","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1283&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/upright-folds\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-116.865864,34.947162]}},{"type":"Feature","properties":{"id":1104,"name":"Kinked foliation","description":"<p>Kinked foliation. Boscastle, Cornwall. UK<br \/>\nPhotoID335<\/p>\n<p>Photograph: Jim Talbot<\/p>\n","modified":"2018-06-30T12:37:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Kinked-foliation-197x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1104","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1104&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/kinked-foliation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.698765,50.691844]}},{"type":"Feature","properties":{"id":1281,"name":"South-verging folds (Samaria Gorge)","description":"<p>Metre-scale south-verging folds in the Plattenkalk nappe. Several faults and these asymmetric south-verging folds (photo) reflect Oligocene compression and are exposed in the Samaria Gorge, which developed as a result of contemporaneous (Pleistocene) continent uplift and erosion.<\/p>\n<p>Approximate location of the outcrop.<\/p>\n<p>Photograph: Koen Van Noten<\/p>\n<p>Reference: Fassoulas C. (2004). Field Guide to the Geology of Crete. Natural History Museum of Crete, Publ., 104p, Heraklio (3th edition)<\/p>\n","modified":"2018-10-10T18:51:56","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-verging-folds-Samaria-Gorge-768x576.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1281","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1281&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/south-verging-folds-samaria-gorge\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[23.9693221449852,35.2549041839846]}},{"type":"Feature","properties":{"id":1279,"name":"Reverse faults (Samaria Gorge, Crete)","description":"<p>Centimetre-scale reverse faults cross-cutting alternating dolomites and silica layers of the Plattenkalk nappe. Faults (photo) and asymmetric south-verging folds reflect Oligocene compression and are exposed in the Samaria Gorge, which developed as a result of contemporaneous (Pleistocene) continent uplift and erosion.<\/p>\n<p>Approximate location of the outcrop<\/p>\n<p>Photograph: Koen Van Noten<\/p>\n<p>Reference: Fassoulas C. (2004). Field Guide to the Geology of Crete. Natural History Museum of Crete, Publ., 104p, Heraklio (3th edition)<\/p>\n","modified":"2018-09-04T13:20:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Reverse-faults-Samaria-Gorge-Crete-768x531.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1279","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1279&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/reverse-faults-samaria-gorge-crete\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[23.954752385616302,35.29608394976411]}},{"type":"Feature","properties":{"id":1277,"name":"Hasan-Robat","description":"<p>The Precambrian Basement of the Hasan-Robat Region, north Isfahan, in the Sanandaj-Sirjan Metamorphic Belt of Iran preserves evidence of multiple orogenic events. The Sanandaj-Sirjan Zone is the inner crystalline zone of the Zagros Orogen, which has been highly deformed and exhumed during continental collision between the Arabian Plate and Central Iran. The Hasan-Robat Region is an example of the exhumed Precambrian basement complexes.<\/p>\n<p>In the photo, deformed Precambrian grey marbles contain metamorphosed chert (cream folded layers) which, record a complex shortening and shearing history. This lead to the development of disharmonic ptygmatic folds with vertical axes during the Pan-African Orogeny and later phases.<br \/>\nLocation: The photo has taken in the southeast Hasan-Robat Village in the north Isfahan, Iran PhotoID222<\/p>\n<p>Nadimi, A., 2010, Journal of Structural Geology, Vol. 32, 263<\/p>\n<p>Photograph: Alireza Nadimi<\/p>\n","modified":"2018-10-10T18:51:45","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Hasan-Robat-768x576.jpg","taxonomy":{"webmapp_category":[228,229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1277","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1277&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/hasan-robat\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[50.91407775878906,33.40253396866421]}},{"type":"Feature","properties":{"id":1271,"name":"Late burial quartz veins","description":"<p>Late burial, bedding-normal extension veins restricted to Lower Devonian sandstones in an overturned fold limb. These quartz veins are similar in orientation prior to folding as the intermullion veins observed in Dedenborn and Bastogne and reflect the early Variscan stress state at the late burial. They formed as a result of high-fluid pressure during extension.<\/p>\n<p>Outcrop excellent for studying vein-rock interactions. Situated at the shores of the Rursee reservoir in the North Eifel (High-Ardenne slate belt, Germany). The outcrops are easy accessible and can be visited the whole year (maximum outcrop capacity in winter).<\/p>\n<p>Van Noten, K., Hilgers, C., Urai, J.L. & Sintubin, M. 2008. Geologica Belgica 11, 179-198.<br \/>\nVan Noten, K. and Sintubin, M. 2010.Journal of Structural Geology 32, 377-391.<br \/>\nVan Noten, K., Muchez, P. & Sintubin, M. (in press). Journal of the Geological Society, London 168, (2011)<br \/>\nPhotoID220<\/p>\n<p>Photograph: Koen Van Noten<\/p>\n","modified":"2019-06-16T21:48:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Late-burial-quartz-veins-768x576.jpg","taxonomy":{"webmapp_category":[224]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1271","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1271&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/late-burial-quartz-veins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.403162479400635,50.630626668845856]}},{"type":"Feature","properties":{"id":1269,"name":"Angular fold train","description":"<p>Angular fold train in a multilayer sequence (chert-limestone) at Agios Pavlos (Crete, Greece).<\/p>\n<p>Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-10-10T18:52:06","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Angular-fold-train-768x576.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1269","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1269&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/angular-fold-train\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[24.562339782714844,35.10178922694953]}},{"type":"Feature","properties":{"id":1267,"name":"Soft-sediment deformation","description":"<p>Chaotic soft-sediment deformation in Upper Carboniferous sandstone-mudstone sequence.<\/p>\n<p>Kenis, I., Vandenberghe, N. & Sintubin, M. 2003. Early Variscan, soft-sediment deformation features in the Chemin de Ronde section at the Namur Citadel (Belgium). Geologica Belgica 6, 161-169.<\/p>\n<p>Photograph: Manuel Sintubin<\/p>\n","modified":"2018-06-15T10:16:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Soft-sediment-deformation-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1267","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1267&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/soft-sediment-deformation\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.865371,50.460178]}},{"type":"Feature","properties":{"id":1265,"name":"Small-scale thrust","description":"<p>Small-scale thrust in a sandstone sequence (Upper Carboniferous), expressing the Late Palaeozoic contraction at the northern Variscan front zone.<\/p>\n<p>Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-06-30T12:31:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Small-scale-thrust-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1265","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1265&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/small-scale-thrust\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.860624074935913,50.457387901484346]}},{"type":"Feature","properties":{"id":1263,"name":"Karakorum Fault","description":"<p>Mylonite, from granitoid rock, along the Karakorum Fault near Pangong (Jammu-Kashmir, India). Foliation is nearly vertical and the sense of shear detected by C-S fabric is dextral (top-to-the SSE sense of shear).<\/p>\n<p>Jain, A.K., Singh, S., 2009. Geology and Tectonics of the Southeastern Ladakh and<br \/>\nKarakoram. In: Geological Society of India, Bangalore, 181 pp.<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2018-06-28T18:12:58","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Karakorum-Fault-768x516.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1263","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1263&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/karakorum-fault\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[78.116941,34.085643]}},{"type":"Feature","properties":{"id":1261,"name":"Mt. Everest","description":"<p>South Tibetan Detachment System, Mount Everest.<br \/>\nThe upper low-angle normal fault of the South Tibetan Detachment System affects the summit of Mt. Everest: the upper dark pyramid on the top is made by Ordovician limesone of the Tethyan Sedimentary Sequence and the brownish rocks below belong to the metamorphic North Col Formation. The rock in the lower part are metamorphic rocks of the Higher Himalayan Crystallines.<br \/>\nView from the south (Rongbuck valley) to the north; the observable height of the northern slope is nearly 4500 m.<\/p>\n<p>Burchfield et al (1992) – Geol. Soc. Am. Spec. Publ., 269, pp. 41.<\/p>\n<p>Carosi et at (1998) – J. Asian Earth Sci., 16, 299-311.<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2019-01-30T18:32:40","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mt.-Everest-300x205.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1261","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1261&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mt-everest\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[86.84394490478519,28.16316938908536]}},{"type":"Feature","properties":{"id":1100,"name":"Fold interference pattern","description":"<p>Refolded isoclinal F1 folds in cherty metalimetsones of the Alpi Apuane metamorphic complex (Northern Appennines, Italy)<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2018-10-10T18:52:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fold-interference-pattern-768x532.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1100","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1100&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/fold-interference-pattern\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[10.214435,44.122228]}},{"type":"Feature","properties":{"id":1259,"name":"refolded crenulation cleavage","description":"<p>This outcrop of micaschist shows a tightly folded spaced foliation of light quartz rich and dark mica rich bands. The regularity of the alternation of the bands suggests that this is not bedding but a tectonic layering. In the quartz-rich layers, a foliation can be seen at a high angle to the layering. If the layering is tectonic, this foliation could be S1 and the layering S2. The foliation S1 is folded (with the layering S2) in the central folds, which must therefore be D3 structures.<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T18:11:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/refolded-crenulation-cleavage-768x500.jpg","taxonomy":{"webmapp_category":[229,232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1259","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1259&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/refolded-crenulation-cleavage\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-4.62569475174,53.27978996944675]}},{"type":"Feature","properties":{"id":1255,"name":"Normal sense shear zone, Bhutan","description":"<p>Normal sense shear zones (top-to-SE) in the hgh-grade gneiss in the core of the Higher Himalayan Crystallines of western Bhutan Himalayas. The age of shearing is 20-17 Ma.<\/p>\n<p>CAROSI R. et al (2006) Geol. Soc. London Spec. Publ., 268, 425-444.<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2018-06-28T18:11:31","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Normal-sense-shear-zone-Bhutan-768x510.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1255","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1255&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/normal-sense-shear-zone-bhutan\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.736734,28.013919]}},{"type":"Feature","properties":{"id":1253,"name":"Detachment folding","description":"<p>Detachment folding in lower Cretaceous coal-bearing strata of the Luscar Group as exposed by mining in the AN pit of the Cardinal River Coal Mine near Hinton, Alberta, Canada. The dragline at the bottom of the pit provides a scale. The Jewel Coal Seam, which has a stratigraphic thickness of 10 m, is structurally thickened in the cores of chevron-type folds, providing enhanced mining situations. There are various detachment horizons. The one visible in the picture is at the contact of the Jewel Coal Seam (black in the centre of the picture) and the underlying sandstone of the Torrens Member. On a larger scale there is detachment along the underlying Folding Mountain\/Mystery Lake Thrust, which in places follows shale horizons in the Nikanassin and Fernie formations. These folds form part of the Cadomin Syncline, which is a footwall syncline of the Nikanassin\/Drinnan Thrust.<\/p>\n<p>Lebel, D., Langenberg, C.W. and Mountjoy, E.W. (1996). Bulletin of Canadian Petroleum Geology 44, 282-298<\/p>\n<p>This is a Journal of Structural Geology Photograph of the Month (JSG 30, 547). Photo ID 201<\/p>\n<p>Photograph: Willem Langenberg<\/p>\n","modified":"2018-07-24T12:28:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Detachment-folding-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1253","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1253&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/detachment-folding\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-117.44258,53.06469]}},{"type":"Feature","properties":{"id":1251,"name":"sandstone dyke","description":"<p>sandstone dyke cutting layering in turbidite. PhotoID199<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-10-10T18:52:49","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/sandstone-dyke-192x300.jpg","taxonomy":{"webmapp_category":[224,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1251","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1251&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/sandstone-dyke\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-70.9208,-53.626001]}},{"type":"Feature","properties":{"id":1249,"name":"Sheath fold in mylonite","description":"<p>The sheath fold in the photograph formed during dextral, southeast-side-up shear along the Assean Lake shear zone. The shear zone dips steeply to the southeast. In general, moderately ENE-plunging lineations in the shear zone are folded by drag folds that have commonly developed into non-cylindrical folds. The lineations and the folds are interpreted as having formed during dextral, southeast-side-up, thinning flow. In this photograph, the lineation on the ESE limb of the fold plunges moderately to the E, and the fold hinge lines plunge steeply to the SSW and shallowly to the NNE. The top of this photograph is towards the WNW. The lineation and fold hinge lines are thought to have partially rotated towards the direction of the maximum principal strain rate of the pure shear component, which may or may not be parallel to the shear direction (cf. Kuiper et al., JSG, 2007)<\/p>\n<p>This is a photograph of the month in JSG<br \/>\nPhotoID198<\/p>\n<p>Photograph: Yvette D. Kuiper<\/p>\n","modified":"2018-06-30T12:57:16","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Sheath-fold-in-mylonite-1-768x576.jpg","taxonomy":{"webmapp_category":[229,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1249","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1249&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/sheath-fold-in-mylonite-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-96.347,56.111]}},{"type":"Feature","properties":{"id":1247,"name":"Mylonitic micaschist","description":"<p>Biotite-sillimanite mylonitic micaschist (Higher Himalayan Cristallines). C-S fabric points to a top-to-the-NE sense of shear due to the activity of the South Tibetan Detachment. PhotoID196<\/p>\n<p>Photograph: chiara Montomoli<\/p>\n","modified":"2018-06-28T14:43:41","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitic-micaschist-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1247","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1247&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mylonitic-micaschist\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.739577,28.188984]}},{"type":"Feature","properties":{"id":1245,"name":"Milonitic leucogranite","description":"<p>Mylonitic leucogranite belonging to the Higher Himalayan Cristallines. C-S fabric, pointing to a top to-the-NE sense of shear, is linked to the South Tibetan Detachment activity. PhotoID195<\/p>\n<p>Photograph: Chiara Montomoli<\/p>\n","modified":"2018-09-04T11:42:48","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Milonitic-leucogranite-768x576.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1245","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1245&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/milonitic-leucogranite\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.740528,28.189117]}},{"type":"Feature","properties":{"id":1243,"name":"South Tibetan Detachment","description":"<p>South Tibetan Detachment dividing the lower Higher Himalayan Crystalline made by leucogranite (white) overlaied by biotite-sillimanite micaschist (grey) from the upper Tibetan Sedimentary Sequence constituded by very low grade metamorphic ordovician limestones. Top to the NE sense of shear. PhotoID194<\/p>\n<p>Photograph: Chiara Montomoli<\/p>\n","modified":"2018-10-10T18:54:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-Tibetan-Detachment-768x576.jpg","taxonomy":{"webmapp_category":[219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1243","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1243&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/south-tibetan-detachment\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.739616,28.189158]}},{"type":"Feature","properties":{"id":1239,"name":"linear mylonites","description":"<p>Ductile greenschist facies shear zone in micaschsit and pegmatite. The shear zone is unusual because it contains linear, constrictional mylonites. PhotoID192<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-09-03T16:55:05","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/linear-mylonites-197x300.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1239","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1239&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/linear-mylonites\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[1.449755430221558,42.646665411846755]}},{"type":"Feature","properties":{"id":1237,"name":"stylolites in marbles","description":"<p>Deformed marbles containing green metachert layers which are transected by multiple stylolites during oblique collision in the Zagros orogenic belt. Subhorizontal sylolites are overpinted by steep ones. It is unclear whether the displacement of layer fragments is solely due to dissolution on stylolites or if it is due to displacement in domino boudinage, with subsequent lateral shortening. PhotoID191<\/p>\n<p>Faghih, A., 2008. Structural evolution of accretion and collision processes of the Zagros orogeny, Iran. Unpublished PhD thesis, Shiraz University,Shiraz , Iran.<br \/>\nSarkarinejad, K., Faghih, A., Grasemann, B., 2008. Transpressional deformations within the Sanandaj-Sirjan Metamorphic Belt (Zagros Mountains, Iran). Journal of Structural Geology 30, 818\u201382<\/p>\n<p>This is a Journal of Structural Geology Photograph of the Month<\/p>\n<p>Photograph:<\/p>\n","modified":"2018-07-24T11:33:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/stylolites-in-marbles-768x575.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1237","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1237&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/stylolites-in-marbles\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[54.221388,29.204444]}},{"type":"Feature","properties":{"id":2150,"name":"Eppelsberg","description":"<p>ring dyke in Eppelsberg scoria cone<br \/>\nPhotoID749<\/p>\n<p>Photograph: Alessandro Da Mommio<\/p>\n","modified":"2018-06-30T12:26:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Eppelsberg-225x300.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/2150","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2150&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/eppelsberg\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[7.320917844772339,50.40261632440939]}},{"type":"Feature","properties":{"id":1416,"name":"South border","description":"<p>Grey: deposits: ashes and bombs deposits from 1888-1890 and 1731-1739 eruptions.<br \/>Orange: surge deposits. Photo ID 658<\/p>\n<p>Photograph: S. Papeschi<\/p>\n","modified":"2018-06-15T10:15:35","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/South-border-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1416","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1416&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/south-border\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[14.960997104644775,38.40203736518958]}},{"type":"Feature","properties":{"id":1235,"name":"Folding in a ductile shear zone","description":"<p>Folded layering in the Deh Vazir ductile shear zone, Iran. This is a structure as described by vanderPluijm and Marshak (1997); folding accompanies shearing and occurs where a sequence of interlayered weak and strong rock layers is caught between the opposing boundaries of a shear zone. In such circumstances, displacement of the rigid shear zone boundaries with respect to each other causes the intervening rock to fold. The Deh Vazir shear zone mainly consists of foliated and lineated marble and greenschist. Metamorphic grade is generally low grade (Sarkarinejad et al., 2010). The photograph shows how strong marble layers act as a shear zone boundary and weak greenschist layers between the marble layers have been subject of shearing. Location: Deh Vazir shear zone in the Southwest of the HP-LT Sanandaj-Sirjan metamorphic belt, Iran. PhotoID190<\/p>\n<p>Sarkarinejad, K., Samani, B., Faghih, A., Grasemann, B., Moradipoor, M., 2010. Implications of strain and vorticity of flow analyses to interpret the kinematics of an oblique convergence event (Zagros Mountains, Iran). Journal of Asian Earth Sciences 38, 34-43<\/p>\n<p>van der Pluijm, B.A., Marshak, S., 1997. Earth Structure: an Introduction to Structural Geology and Tectonics, McGraw-Hill, New York.<\/p>\n<p>This is a photograph of the month in the Journal of Structural Geology<\/p>\n<p>Photograph: Babak Samani<\/p>\n","modified":"2018-10-10T18:54:20","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folding-in-a-ductile-shear-zone-768x576.jpg","taxonomy":{"webmapp_category":[229,219,231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1235","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1235&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/folding-in-a-ductile-shear-zone\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[54.793333,29.342222]}},{"type":"Feature","properties":{"id":1233,"name":"Disharmonic folds, Marble Point","description":"<p>Disharmonic folds in marbles deformed during the Ross Orogeny, Marble Point, Victoria Land (Antarctica). PhotoID187<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2018-10-10T18:53:01","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Disharmonic-folds-Marble-Point-300x192.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1233","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1233&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/disharmonic-folds-marble-point\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.833,-77.433]}},{"type":"Feature","properties":{"id":1231,"name":"Folds in marbles, Dry Valleys","description":"<p>Tight folds with stretched limbs in quartz-feldspatic layer in high-grade marbles, Roos Orogen. Nussbaun Riegel, Taylor Valley, Victoria Land (Antarctica). PhotoID186<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2018-09-03T14:16:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Folds-in-marbles-Dry-Valleys-225x300.jpg","taxonomy":{"webmapp_category":[228,229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1231","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1231&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/folds-in-marbles-dry-valleys\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.76666,-77.66666]}},{"type":"Feature","properties":{"id":1229,"name":"Asymmetric boudins, Dry Valleys","description":"<p>Asymmetric boudins of a quartz-feldspatic layer within high-grade marbles, Ross Orogen. Nussbaum Riegel, Dry Valleys (Taylor Valley), Victoria Land (Antarctica). PhotoID185<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2018-06-28T14:50:26","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Asymmetric-boudins-Dry-Valleys-e1530184771899-768x576.jpg","taxonomy":{"webmapp_category":[228]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1229","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1229&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/asymmetric-boudins-dry-valleys\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[162.76665,-77.66666]}},{"type":"Feature","properties":{"id":1227,"name":"Fold interference at Contortion Spur","description":"<p>Type 3 fold interference between F2 open folds and tight F1 folds (lower part of the photograph) in Cambrian Sequence of the Selborne Group (Ross Orogen) at Contortion Spur (Byrd Glacier, Antarctica). Dark rocks are Contortion schists whereas whitish rocks are Madison Marble. The height of the southern slope of Mt. Madison is nearly 500 m. Helicopter view. PhotoID182<\/p>\n<p>CAROSI et al (2007) USGS OF-2007-1047, Short Research Paper 030; doi:10.3133\/of2007-1047.srp030.<\/p>\n<p>Stump et al (2004) New Zealand Journal of Geology and Geophysics, Vol. 47: 157\u2013171<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2018-06-28T18:09:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Fold-interference-at-Contortion-Spur-225x300.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1227","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1227&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/fold-interference-at-contortion-spur\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[160.18407935999994,-80.4093906241]}},{"type":"Feature","properties":{"id":1223,"name":"F2 folds, Tukuche Peak","description":"<p>Overturned F2 folds on the south-eastern slope of Tukuche Peak (6950 m) affecting Ordovician to Devonian succession of the Tethyan Sedimentary Sequence (Kali Gandaki valley, Nepal). Height of the slope is >3000 m. PhotoID179<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2019-01-07T12:53:55","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/F2-folds-Tukuche-Peak-768x516.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1223","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1223&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/f2-folds-tukuche-peak\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[83.7661927947388,28.79535103893526]}},{"type":"Feature","properties":{"id":1221,"name":"lava tunnel on Reunion","description":"<p>lava tunnel on the island of reunion. 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Photo ID 657<\/p>\n<p>Photograph: S. 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In the background a dam in the river is visible which was uplifted on the thrust as well, and which shows damage at left where teh fault cut the dam body. Uplift associated with the 1999 earthquake. PhotoID173<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-15T10:15:13","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/waterfall-caused-by-fault-scarp-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1213","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1213&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/waterfall-caused-by-fault-scarp\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[120.76036405563354,24.27956159054501]}},{"type":"Feature","properties":{"id":1211,"name":"Earthquake damage to dam","description":"<p>Damage to the Shih-Kang dam, the first dam in the world ever to be directly deformed by a earthquake surface rupture. 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PhotoID172<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-10-10T18:54:30","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Earthquake-damage-to-dam-768x576.jpg","taxonomy":{"webmapp_category":[220,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1211","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1211&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/earthquake-damage-to-dam\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[120.76859307289124,24.28271066985509]}},{"type":"Feature","properties":{"id":1405,"name":"View of fumaroles and crater area","description":"<p>Photo shot from the South border of the crater. 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On the right a Bread-crust bomb is visible. Photo ID 655<\/p>\n<p>Photograph: S. 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Here, folations are not simply axial planar; in some cases there seem to be two axial planar crenulations overprinting each other within thier parent fold closure. Williams 1971. J geol Soc Australia 18, 215-228; Powell and Rickard 1985 JSG 7, 385-400. PhotoID170<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-28T14:38:21","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bermagui-Fold-768x481.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1209","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1209&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/bermagui-fold\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[150.07447063922882,-36.4220270543]}},{"type":"Feature","properties":{"id":1207,"name":"Domino faults","description":"<p>The photograph shown antitetic domino-microfaults in the so called Parvenets two-mica plagiogneisses which consitute the basement of the Trakia unit, northern Central Rhodopes, Bulgaria. The antitetic domino-microfaults indicate top-o-the-left (top-to-the southeast) sense of shear. These faults are formed during the third deformation phase in the tectonic evolution of the area \u2013 a stage of brittle to brittle-ductile strike-slip faulting and south-vergent trusting. During this stage some parts of the Trakia unit overtrusted the Late Oligocene sediments from the northernmost slopes of the Central Rhodopes. Near Parvenets village in the area of Plovdiv. PhotoID169<\/p>\n<p>Photograph: Kalin V. Naydenov<\/p>\n","modified":"2019-01-28T15:16:19","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Domino-faults-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1207","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1207&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/domino-faults\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[24.57416699999999,41.601111]}},{"type":"Feature","properties":{"id":1205,"name":"Sheath fold in mylonite","description":"<p>The sheath fold in the photograph formed during dextral, southeast-side-up shear along the Assean Lake shear zone. The shear zone dips steeply to the southeast. In general, moderately ENE-plunging lineations in the shear zone are folded by drag folds that have commonly developed into non-cylindrical folds. The lineations and the folds are interpreted as having formed during dextral, southeast-side-up, thinning flow. In this photograph, the lineation on the ESE limb of the fold plunges moderately to the E, and the fold hinge lines plunge steeply to the SSW and shallowly to the NNE. The top of this photograph is towards the WNW. The lineation and fold hinge lines are thought to have partially rotated towards the direction of the maximum principal strain rate of the pure shear component, which may or may not be parallel to the shear direction (cf. Kuiper et al., JSG, 2007). PhotoID168<\/p>\n<p>This is a Photograph of the Month in the Journal of Structural Geology<\/p>\n<p>Photograph: Yvette D. 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PhotoID167<\/p>\n<p>Photograph: R Carosi<\/p>\n","modified":"2018-06-30T16:19:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mylonitic-orthogneiss-768x516.jpg","taxonomy":{"webmapp_category":[231]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1203","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1203&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mylonitic-orthogneiss\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[87.244983,27.486396]}},{"type":"Feature","properties":{"id":1201,"name":"Nojima fault","description":"<p>The surface rupture along the Nojima fault, following the January 17, 1995 Kobe (Great Hanshin) earthquake, preserved in the Nojima Fault Preservation Museum. 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PhotoID164<\/p>\n<p>Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-06-28T14:49:39","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/antiform-768x576.jpg","taxonomy":{"webmapp_category":[229]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1199","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1199&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/antiform\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[4.863488674163818,50.458854987663635]}},{"type":"Feature","properties":{"id":1197,"name":"quartz veins and mullions","description":"<p>layer-parallel multilayer buckling (mullion development) pinned by pre-existing layer-perpendicular quartz veins.<br \/>\nPhotoID163<br \/>\n– Kenis, I. & Sintubin, M. 2007. About boudins and mullions in the Ardenne-Eifel area (Belgium, Germany). Geologica Belgica 10(1-2), 79-91 (and references therein).<br \/>\n– Sintubin, M. 2008. Photograph of the month: Boudin centennial. Journal of Structural Geology 30, 1315-1316 (doi: 10.1016\/j.jsg.2008.06.003).<\/p>\n<p>Photograph: Manuel Sintubin (K.U.Leuven, Belgium)<\/p>\n","modified":"2018-10-10T18:54:43","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/quartz-veins-and-mullions-1-768x516.jpg","taxonomy":{"webmapp_category":[229,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1197","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1197&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/quartz-veins-and-mullions-2\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.84072470664978,50.090705354465136]}},{"type":"Feature","properties":{"id":1195,"name":"Geologist on Elephant Island","description":"<p>Typical coastal cliff of micaschist on Elephant Island with overhaning glacier. The cliffs are due to recent uplift of the island. Sampling is only possible by quickly slipping below the glacier and hoping that no piece will break off at that time. Notice size of geologist dressed in yellow at the foot of the cliff. PhotoID162<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2019-01-28T15:17:50","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Geologist-on-Elephant-Island-674x1024.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1195","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1195&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/geologist-on-elephant-island\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-55.10039786054688,-61.19143055411936]}},{"type":"Feature","properties":{"id":1343,"name":"COLUMNAR JOINTING IN BASALT","description":"<p>Basalt columns and columnar joints converge upwards in a Tertiary volcanic vent with an age about 14.07\u00b10.37 Ma (K-Ar age, whole rock), north of Jijiazhuang village in the Chnagle area, Shandong province, China. Attitude of these converged BCCJ are possible related to upward conflux of basalt magma. PhotoID159<\/p>\n<p>Photograph: Xing-Wang Xu<\/p>\n<p>Reference: This is a Journal of Structural Geology Photograph of the Month (JSG in press)<\/p>\n","modified":"2018-09-04T15:52:24","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/COLUMNAR-JOINTING-IN-BASALT-768x521.jpg","taxonomy":{"webmapp_category":[224,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1343","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1343&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/columnar-jointing-in-basalt\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[118.79583,36.5561]}},{"type":"Feature","properties":{"id":1193,"name":"Pseudotachylyte","description":"<p>Pseudotachylyte at teh base of the Perry Sound Allochthone<br \/>\nFresh rock cuts created recently during selective upgrading of Highway 522 in Golden Valley village and its vicinity facilitate the detailed study of Grenvillian structures. In western outskirts of Golden Valley village, pseudotachylite veins and breccias are discernible on clean outcrop surfaces of highly strained granodiorite-tonalite gneiss marking the basal contact of the Parry Sound allochthon (Davidson et al., 1982; Culshaw et al., 1997; Wodicka et al., 2000). As at various localities along the Georgian Bay shore, eastern Lake Huron (Tony Davidson and Rebecca Jamieson, written communications), the presence of pseudotachylite veins and breccias attests to seismic failure and friction melting near the basal contact of the Parry Sound allochthon, at middle to shallow crustal levels<\/p>\n<p>Davidson, A., Culshaw, N.G., Nadeau, L., 1982. A tectono-metamorphic framework for part of the Grenville Province, Ontario. Geological Survey of Canada Paper 82-1A, 275 \u2013 290.<br \/>\nCulshaw, N.G., Jamieson, R.A., Ketchum, J.W.F., Wodicka, N., Corrigan, D., Reynolds, P.H., 1997. Transect across the southwestern Grenville Orogen, Georgian Bay, Ontario: polystage convergence and extension in the lower orogenic crust. Tectonics 16, 966 \u2013 982.<br \/>\nJSG Photograph of the Month<\/p>\n<p>Wodicka, N., Ketchum, J.W.F., Jamieson, R.A., 2000. Grenvillian metamorphism of<br \/>\nmonocyclic rocks, Georgian Bay, Ontario, Canada: implications for convergence<br \/>\nhistory. Canadian Mineralogist 38, 471 \u2013 510. PhotoID161<\/p>\n<p>Photograph: Fried Schwerdtner<\/p>\n","modified":"2018-09-03T17:28:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pseudotachylyte-768x576.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1193","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1193&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/pseudotachylyte\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-79.819633,45.920616]}},{"type":"Feature","properties":{"id":1189,"name":"Amphibolite boudin","description":"<p>Metric-size boudin of massive hornblende-plagioclase amphibolites in the migmatites of the Variscan basement of Asinara island (Italy) PhotoID158<\/p>\n<p>CAROSI R, DI PISA A., IACOPINI D., MONTOMOLI C, OGGIANO G. (2004) – The structural evolution of the Asinara Island (NW Sardinia, Italy). Geodinamica Acta, 17, 5 309-329, Lovoisier Parigi.<\/p>\n<p>CAROSI R., FRASSI C., MONTOMOLI C., IACOPINI D. (2006) – Excursion in the Variscan Basement of Northern Sardinia (Italy): Field Guide. In: (eds.) K\u00f6hn, D., and De Paor, D., General Contributions 2006, Journal of the Virtual Explorer, Electronic Edition, ISSN 1441-8142, Volume 22, Paper 3.<\/p>\n<p>Photograph: R. 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Usually andalusite grows during a HT-LP metamorphic event after staurolite. PhotoID157<\/p>\n<p>Photograph: R. Carosi<\/p>\n","modified":"2018-10-10T18:55:27","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Andalusite-bearing-micaschist-300x225.jpg","taxonomy":{"webmapp_category":[234,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1187","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1187&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/andalusite-bearing-micaschist\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[8.259208679199219,41.05718945133737]}},{"type":"Feature","properties":{"id":1098,"name":"Bermagui","description":"<p>coastal outcrops of slate in Bermagui – this is a classical site to study the development of foliations in slates and sandstones. PhotoID171<\/p>\n<p>Photograph: Cees Passchier<\/p>\n","modified":"2018-06-30T11:14:10","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Bermagui-768x481.jpg","taxonomy":{"webmapp_category":[232]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1098","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1098&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/bermagui\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[150.08198082447052,-36.4227522334]}},{"type":"Feature","properties":{"id":1185,"name":"Mullions at Dedenborn, Germany","description":"<p>Small roadside outcrop near the village of Dedenborn in the N-Eifel, the type example of mullions.<\/p>\n<p>The outcrop is situated in the steep to overturned limb of a regional series of upright folds with well-developed axial planar cleavage. The rocks consist of alternating psammite-pelite layers.<\/p>\n<p>Janos Urai, G. Spaeth, Wouter van der Zee, Christoph Hilgers (2001). Evolution of mullion (boudin) structures in the Variscan of the Ardennes and Eifel. Journal of the Virtual Explorer online, 3,1<br \/>\n*Ilse Kenis, Janos Urai, Wouter van der Zee, Christoph Hilgers, Manuel Sintubin (2005). Rheology of fine-grained siliciclastic rocks in the middle crust \u2013 evidence from a combined structural and numerical analysis. Earth and Planetary Science Letters, 233,351-360<\/p>\n<p>http:\/\/www.ged.rwth-aachen.de\/index.php?cat=Research&subcat=Fractures_and_veins&page=Mullions_and_Boudins PhotoID156<\/p>\n<p>Photograph: Heijn van Gent<\/p>\n","modified":"2018-06-28T18:05:08","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mullions-at-Dedenborn-Germany-225x300.jpg","taxonomy":{"webmapp_category":[220,232,230]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1185","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1185&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mullions-at-dedenborn-germany\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[6.352341,50.581511]}},{"type":"Feature","properties":{"id":1183,"name":"Original boudin locality","description":"<p>This old quarry is the locality where in 1908 the terms boudin and boudinage were coined: \u2018\u2018Lorsque l\u2019on voit ces segments renfl\u00e9s sur une surface de stratification \u00e9tendue, mise \u00e0 nu par l\u2019exploitation, on croirait voir une s\u00e9rie d\u2019\u00e9ormes cylindres ou boudins align\u00e9s c\u00f4t\u00e9 \u00e0 c\u00f4t\u00e9 …<br \/>\nsur l\u2019initiative de M. Lohest on a fr\u00e9quemment utilis\u00e9, pour la facilit\u00e9 du langage, les n\u00e9ologismes de boudiner et de boudinage.\u2019\u2019<\/p>\n<p>Lohest, M., Stainier, X., Fourmarier, P., 1908. Compte rendu de la session extraordinaire<br \/>\nde la Soci\u00e9t\u00e9 G\u00e9ologique de Belgique, tenue \u00e0 Eupen et \u00e0 Bastogne les 29,<br \/>\n30et 31 ao\u00fbt et le 1, 2 et 3 septembre 1908. Annales de la Soci\u00e9t\u00e9 g\u00e9ologique de<br \/>\nBelgique 35, B351\u2013B434. PhotoID153<\/p>\n<p>Photograph: Manuel Sintubin<\/p>\n","modified":"2018-06-28T14:34:44","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Original-boudin-locality-768x1024.jpg","taxonomy":{"webmapp_category":[228]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1183","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1183&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/original-boudin-locality\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.736709982156754,50.00788467662985]}},{"type":"Feature","properties":{"id":1181,"name":"quartz veins and mullions","description":"<p>Metasandstone-metapelite multilayer sequence with regularly spaced layer-perpendicular quartz veins and buckled interfaces, Carri\u00e8re Mardasson, Bastogne.PhotoID152<br \/>\nThis is one of the localities where in 1908 the terms boudin and boudinage were coined.<br \/>\nThis quarry can only be visited by appointment.<\/p>\n<p>Photograph: Manuel Sintubin<\/p>\n<p>Reference: Sintubin, M. 2008. Photograph of the month: Boudin centennial. Journal of Structural Geology 30, 1315-1316 (doi: 10.1016\/j.jsg.2008.06.003)<\/p>\n","modified":"2018-10-23T13:50:23","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/quartz-veins-and-mullions-768x576.jpg","taxonomy":{"webmapp_category":[228,229,224,219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1181","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1181&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/quartz-veins-and-mullions\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[5.742212533950806,50.01537834744035]}},{"type":"Feature","properties":{"id":1179,"name":"Magmatic stoping (Costa Brava)","description":"<p>The north cliff of Cala Pedrosa: a unique example of multiple granitoid emplacement by the magmatic stoping mechanism in the Variscan Costa Brava batholith. The darkest rocks (hornfels) were first intruded by a granodioritic magma (grey) and both the hornfels and the solidified granodiorite were subsequently intruded by leucogranites (light coloured rocks). Moreover, the whole set of rocks is cut by a lamprophyric dyke (lower left). PhotoID151<\/p>\n<p>Photograph: Elena Druguet<\/p>\n<p>Reference: mediambient.gencat.cat\/Images\/43_39667.pdf<\/p>\n","modified":"2018-06-15T10:14:36","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Magmatic-stoping-Costa-Brava-768x576.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1179","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1179&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/magmatic-stoping-costa-brava\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[3.218657,41.935562]}},{"type":"Feature","properties":{"id":1177,"name":"Hydrothermal Breccia","description":"<p>Hidden Valley is formed by about 10 square km of hydrothermal breccia. 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PhotoID147<\/p>\n<p>Photograph: Paul Bons<\/p>\n","modified":"2018-06-15T10:14:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Hydrothermal-Breccia-300x200.jpg","taxonomy":{"webmapp_category":[219]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1177","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1177&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/hydrothermal-breccia\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[139.52102422714233,-30.0691682442]}},{"type":"Feature","properties":{"id":1175,"name":"Antitaxial veins","description":"<p>Fibrous, antitaxial calcite veins are abundant in the slates of the Neoproterozic Tapley Hill Formation. These 585 Ma veins may contain the so far oldest fossil remains of deep microbial life<\/p>\n<p>Bons, P.D. (2009) Photograph of the month. Journal of Structural Geology 31, 627-627.<br \/>\nBons, P.D., Montenari, M., Bakker, R.J., Elburg, M.A. (2008) Potential evidence of Neoproterozoic deep life: SEM observations on calcite veins from Oppaminda Creek, Arkaroola, South Australia. International Journal of Earth Sciences 98, 327-343<br \/>\nBons, P.D. Montenari, M. 2005. The formation of antitaxial calcite veins with well developed fibres, Oppaminda Creek, South Australia. Journal of Structural Geology 27, 231-248. PhotoID146<\/p>\n<p>Photograph: Paul Bons<\/p>\n","modified":"2018-06-30T11:48:04","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Antitaxial-veins-768x512.jpg","taxonomy":{"webmapp_category":[224]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1175","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1175&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/antitaxial-veins\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[139.3976855278015,-30.3241932576]}},{"type":"Feature","properties":{"id":1173,"name":"Mulgandinnah shear zone","description":"<p>3Ga deformation of the Mulgandinnah shear zone in Archaean gneisses of the Shaw Batholith, Pilbara. PhotoID143<\/p>\n<p>Photograph: C. W. 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PhotoID142<\/p>\n<p>Photograph: AChanou<\/p>\n","modified":"2018-10-10T18:57:34","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Pissia-fault-scarp-768x574.jpg","taxonomy":{"webmapp_category":[220]},"accessibility":{"mobility":{"check":false,"description":""},"hearing":{"check":false,"description":""},"vision":{"check":false,"description":""},"cognitive":{"check":false,"description":""},"food":{"check":false,"description":""}},"locale":"it","source":"https:\/\/outcropedia.tectask.org\/wp-json\/wp\/v2\/poi\/1171","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=1171&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/pissia-fault-scarp\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[22.98811912536621,38.01656569516094]}},{"type":"Feature","properties":{"id":1169,"name":"sag pond","description":"<p>Saline lake in a sag pond formed by fault reactivation of a Proterozoic shear zone, probably assocaited with Lake Baikal rifting. 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This small outcrop underneath the footbridge to the church shows very nice examples of type III fold interference. Take care, the outcrop is slippery and can only be reached along a narrow path! 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