File:Kames in the plain of Kinross - geograph.org.uk - 354057.jpg

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English: Kames in the plain of Kinross The plain of Kinross, despite being over 100 metres above sea level, is one of the flattest-lying areas of Central Scotland. It contains abundant evidence of recent glaciation, of which these low knolls are examples. Known as Kames, they were formed by the accumulation of rock fragments in hollows in the surface of the glaciers during the final retreat of the ice-sheets about 10,000 years ago.
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Source From geograph.org.uk
Author Brendan Hamill
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Brendan Hamill / Kames in the plain of Kinross / 
Brendan Hamill / Kames in the plain of Kinross
Camera location56° 11′ 36″ N, 3° 27′ 37″ W  Heading=315° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location56° 11′ 40″ N, 3° 27′ 46″ W  Heading=315° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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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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current19:16, 2 January 2011Thumbnail for version as of 19:16, 2 January 2011640 × 480 (91 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Kames in the plain of Kinross The plain of Kinross, despite being over 100 metres above sea level, is one of the flattest-lying areas of Central Scotland. It contains abundant evidence of recent gla

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