File:Omarama Clay Cliffs en 2010.jpg
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Français : Les falaises d'argile d'Omaraman, sont d'énormes pinacles et crêtes pointus avec des ravins profonds et étroits les séparant. Les falaises d'argile sont constituées de couches de gravier et de limon, déposées par des rivières s'écoulant des glaciers qui existaient il y a 1 à 2 millions d'années. Comparées aux montagnes voisines, vieilles de 250 millions d'années, les falaises d'argile sont relativement récentes. Aujourd'hui, les couches de gravier et de limon peuvent être considérées comme des bandes inclinées, car les strates ont été inclinées depuis leur dépôt il y a 1 à 2 millions d'années. |
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| Source | Own work | ||||||||||||||||||||
| Author | Pierre André Leclercq | ||||||||||||||||||||
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| Camera location |  | View this and other nearby images on: OpenStreetMap |  |
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This illustration was made by Pierre André Leclercq, under the License CC-BY-SA which allows you to:
Under this condition Credit me as the original author and use the same license. I encourage distribution and modification of this image as long as you attribute its author and license. If you are using one of my images or wish to contact me, please inform me by writing a short message on my discussion page. An email |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 10:18, 22 December 2021 | | 3,456 × 2,592 (5.62 MB) | Pierre André Leclercq (talk | contribs) | Uploaded own work with UploadWizard |
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