File:Glacial meltwater channel below Deuchrie Dod - geograph.org.uk - 1603099.jpg
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English: Glacial meltwater channel below Deuchrie Dod This valley, Rammer Cleugh, is one of several trending roughly E-W on the northern side of the Lammermuir Hills, that are thought to have been formed by meltwater drainage underneath or at the margins of a great glacier that occupied what is now the Firth of Forth. The valleys are striking in the way they cut across the landscape and yet contain no significant streams or rivers.
This is a particularly good example of a landscape modified while it was beneath the ice. For more background including a map of the meltwater channels, please see http://www.fettes.com/lothian/Rammer%20Cleugh.htm |
| Date | |
| Source | From geograph.org.uk |
| Author | Jim Barton |
| Attribution (required by the license) | Jim Barton / Glacial meltwater channel below Deuchrie Dod / |
| 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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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 Jim Barton 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: Jim Barton
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
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| current | 06:25, 4 March 2011 | | 640 × 424 (111 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=Glacial meltwater channel below Deuchrie Dod This valley, Rammer Cleugh, is one of several trending roughly E-W on the northern side of the Lammermuir Hills, that are thought to have been formed by |
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