File:River Terrace - geograph.org.uk - 344078.jpg
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| Description |
English: River Terrace During the Quaternary period, the valley of the R.Ayr was filled by ice which deposited a considerable depth of glacial till. As the ice melted with a return to warmer conditions, huge volumes of meltwater were released along the centre of the valley and eroded the glacial till down to the present floodplain level. At the valley sides these generally flat surfaces were left to show where there had existed an earlier floodplain.
In the background can be seen Nethershield Farm and the present land use of the dissected river terrace on the northern side of the Ayr valley east of Sorn. |
| Date | |
| Source | From geograph.org.uk |
| Author | Bob Forrest |
| Attribution (required by the license) | Bob Forrest / River Terrace / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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_heading:45.00&language=en){kind=link}
| Object location | | View this and other nearby images on: OpenStreetMap | |
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_heading:45.00&language=en){kind=link}
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 Bob Forrest 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: Bob Forrest
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 17:46, 2 January 2011 | | 640 × 426 (59 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=River Terrace During the Quaternary period, the valley of the R.Ayr was filled by ice which deposited a considerable depth of glacial till. As the ice melted with a return to warmer conditions, huge |
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