File:Stowe's Hill - geograph.org.uk - 523006.jpg

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Stowe's_Hill_-_geograph.org.uk_-_523006.jpg(640 × 427 pixels, file size: 121 KB, MIME type: image/jpeg)

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English: Stowe's Hill When granite gets close to the surface it cracks in a rectangular pattern. These cracks get filled with water which starts the process of weathering both by chemical reactions and the effect of freezing and thawing, which would have been a major factor in the ice age. Over the course of time the granite is weathered away and the remaining granite blocks start the slow process of moving down the hillside along with the soil, another process which is helped along in cold periglacial conditions. Under the right conditions, where the granite is particularly hard and the cracks in the granite far apart large boulder stacks like these can be left standing on the hillside, the cores of granite blocks too large to be moved by natural processes. The stack on the right of the photo is the famous Cheesewring.
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Source From geograph.org.uk
Author Tony Atkin
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Tony Atkin / Stowe's Hill / 
Tony Atkin / Stowe's Hill
Camera location50° 31′ 26″ N, 4° 27′ 35″ W  Heading=0° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location50° 31′ 31.8″ N, 4° 27′ 34″ W  Heading=0° 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: Tony Atkin
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current17:36, 5 February 2011Thumbnail for version as of 17:36, 5 February 2011640 × 427 (121 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Stowe's Hill When granite gets close to the surface it cracks in a rectangular pattern. These cracks get filled with water which starts the process of weathering both by chemical reactions and the

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