File:Stream in Biddlecombe - geograph.org.uk - 184768.jpg

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English: Stream in Biddlecombe. The stream is fed by numerous springs which rise along the combe sides and at its head. The combe itself is a result of a geological fault (Biddle Fault) The bedrock changes from Devonian Old Red Sandstone, to Carboniferous limestone and finally Dolomitic Conglomerate as you descend the combe from north to south.
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Source From geograph.org.uk
Author Sharon Loxton
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Sharon Loxton / Stream in Biddlecombe / 
Sharon Loxton / Stream in Biddlecombe
Object location51° 13′ 19″ N, 2° 37′ 16″ W  Heading=180° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo


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Attribution: Sharon Loxton
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current18:45, 31 January 2010Thumbnail for version as of 18:45, 31 January 2010480 × 640 (132 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Stream in Biddlecombe. The stream is fed by numerous springs which rise along the combe sides and at its head. The combe itself is a result of a geological fault (Biddle Fault) The bedrock changes

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