File:Glacial overflow channel - geograph.org.uk - 303466.jpg
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Summary[edit]
| Description |
English: Glacial overflow channel This steep sided (and in places craggy) valley is just below its watershed and has no stream flowing through it at present. It was probably formed towards the end of the last ice age by torrents of water escaping from the melting glaciers. Further down the small Backharn Burn develops, but its present size is too small to have eroded such a substantial valley. |
| Date | |
| Source | From geograph.org.uk |
| Author | Roy Turnbull |
| Attribution (required by the license) | Roy Turnbull / Glacial overflow channel / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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_heading:337.00&language=en){kind=link}
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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 Roy Turnbull 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: Roy Turnbull
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 21:52, 22 December 2010 | | 640 × 480 (113 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Glacial overflow channel This steep sided (and in places craggy) valley is just below its watershed and has no stream flowing through it at present. It was probably formed towards the end of the las |
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