Flexural slip folding in the Canadian Rockies of Alberta, west of Calgary. The Canadian Rockies are part of the North American Cordillera, a mountain belt that extends southward from Alaska along the plate margin. Uplift of this range occurred from late Jurassic through early Cenozoic. Deformed rocks are Carboniferous carbonates. Photo ID 697<\/p>\n
Photograph: David Manaker<\/p>\n
Reference: Eyles & Miall, 2007, Canada Rocks, 512 pages.<\/p>\n","modified":"2018-06-15T10:29:12","color":"","icon":"","noDetails":false,"noInteraction":false,"image":"https:\/\/outcropedia.tectask.org\/wp-content\/uploads\/2018\/06\/Mt.-Kidd-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\/2090","wp_edit":"http:\/\/outcropedia.tectask.org\/wp-admin\/post.php?post=2090&action=edit","web":"https:\/\/outcropedia.tectask.org\/poi\/mt-kidd\/","addr:street":"","addr:housenumber":"","addr:postcode":"","addr:city":"","contact:phone":"","contact:email":"","opening_hours":"","capacity":""},"geometry":{"type":"Point","coordinates":[-115.200076,50.872116]}}