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Original file (2,400 × 1,629 pixels, file size: 1.36 MB, MIME type: image/jpeg)
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Summary
| Description | Many Coronation sills, part of the 723 million year old Franklin Igneous Magmatic Event, slice through the Earth's crust in the western Arctic of Nunavut. Here, at the entrance to Bathurst Inlet, an island-topping sill cuts through Proterozoic rock, a light-coloured carbonate formation in this case. The beautifully layered sand beach is caused by glacial rebound of the Arctic coastline during the current glacial interlude. Little to no tide hereabouts helped to form its layercake look. Isostatic rebound is still underway. | |||
| Date | ||||
| Source |
rebounding beach, among other things
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| Author | Mike Beauregard from Nunavut, Canada | |||
| Other versions |
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| Camera location |  | View this and other nearby images on: OpenStreetMap |  |
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Licensing
This file is licensed under the Creative Commons Attribution 2.0 Generic license.
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This image, originally posted to Flickr, was reviewed on 5 September 2013 by the administrator or reviewer File Upload Bot (Magnus Manske), who confirmed that it was available on Flickr under the stated license on that date. |
File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 04:14, 5 September 2013 | | 2,400 × 1,629 (1.36 MB) | File Upload Bot (Magnus Manske) | Transferred from Flickr by User:PDTillman |
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