File:Gelly Burn and glacial Kame - geograph.org.uk - 354076.jpg
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| Description |
English: Gelly Burn and glacial Kame The low mound is a glacial feature known as a Kame, formed by the accumulation of rock fragments in hollows in the ice surface prior to the final melting of the glaciers which covered this area about 10,000 years ago. |
| Date | |
| Source | From geograph.org.uk |
| Author | Brendan Hamill |
| Attribution (required by the license) | Brendan Hamill / Gelly Burn and glacial Kame / |
| Camera location |   | View this and other nearby images on: OpenStreetMap |  |
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_heading:337.00&language=en){kind=link}
| Object 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 Brendan Hamill 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: Brendan Hamill
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 19:07, 2 January 2011 | | 640 × 480 (100 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Gelly Burn and glacial Kame The low mound is a glacial feature known as a Kame, formed by the accumulation of rock fragments in hollows in the ice surface prior to the final melting of the glaciers |
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