File:Rapid erosion at Chilling Cliff - geograph.org.uk - 1606412.jpg

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English: Rapid erosion at Chilling Cliff. This is a very active section of the coast. Since the summer of 2005 the rate of erosion as reported by the School of Ocean and Earth Science at Southampton University has been measured at 2 metres per annum. One of the observation posts, shown in Peter Facey's picture 91689, taken in 2005 is no longer there. Talus, forming below this cliff is transported east by longshore drift and has formed a bank, diverting the course of the stream from Brownwich Pond, turning it through almost 90 degrees as can be seen in Graham Horn's picture 1145130.
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Source From geograph.org.uk
Author Martin Speck
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Martin Speck / Rapid erosion at Chilling Cliff / 
Martin Speck / Rapid erosion at Chilling Cliff
Camera location50° 49′ 37″ N, 1° 16′ 04″ W  Heading=315° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location50° 49′ 38″ N, 1° 16′ 05″ 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: Martin Speck
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current07:12, 4 March 2011Thumbnail for version as of 07:12, 4 March 2011640 × 480 (85 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Rapid erosion at Chilling Cliff This is a very active section of the coast. Since the summer of 2005 the rate of erosion as reported by the School of Ocean and Earth Science at Southampton Universit

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