File:Sedimentary rocks at the Bendricks - geograph.org.uk - 6589292.jpg
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English: Sedimentary rocks at the Bendricks
“ During the Late Triassic it is probable that the Bendrick Rock area was a low lying marginal environment, where large ephemeral fluvial (river and stream) systems sporadically filled a larger, heavily evaporated, hypersaline lake. The fluvial deposits are interpreted as the result of periodic flash flood events and show a range of sediments and depositional structures. The rivers that existed in this area would have periodically filled the lakes and during times of heavy rainfall burst their banks creating extensive shallow floodplains. These flood events would have deposited fine muds over a wide area and left many shallow pools of rapidly evaporating water.“ [The Geological Society] |
| Date | |
| Source | From geograph.org.uk |
| Author | Alan Hughes |
| Permission (Reusing this file) |
Creative Commons Attribution Share-alike license 2.0 |
| Attribution (required by the license) | Alan Hughes / Sedimentary rocks at the Bendricks / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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| Object location | | View this and other nearby images on: OpenStreetMap | |
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Licensing[edit]
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This image was taken from the Geograph project collection. See this photograph's page on the Geograph website for the photographer's contact details. The copyright on this image is owned by Alan Hughes and is licensed for reuse under the Creative Commons Attribution-ShareAlike 2.0 license.
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This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: Alan Hughes
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 09:19, 13 September 2020 | | 2,048 × 1,536 (1.66 MB) | Geograph Update Bot (talk | contribs) | Higher-resolution version from Geograph. |
| 20:09, 8 September 2020 |  | 1,024 × 768 (351 KB) | Salen9 (talk | contribs) | == {{int:filedesc}} == {{Information |Description={{en|1=Sedimentary rocks at the Bendricks “ During the Late Triassic it is probable that the Bendrick Rock area was a low lying marginal environment, where large ephemeral fluvial (river and stream) systems sporadically filled a larger, heavily evaporated, hypersaline lake. The fluvial deposits are interpreted as the result of periodic flash flood events and show a range of sediments and depositional structures. The rivers that existed in th... |
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