File:Ephemeral Channel - geograph.org.uk - 315333.jpg

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English: Ephemeral Channel Pipeflow and interflow combine, with surface runoff between heather ling clumps and peat mounds, to form an ephemeral channel migrating down channel. This moves forward on the drier soils, the stream advancing in form. Peaty podzol, East Twin Brook, Blackdown Hills ORS, Mendip. source Research:

MD Stagg University of Bristol thesis copyright 1973 and DR Weyman MJ Kirkby LF Curtis 1969 and 1970. That which stuns me is the erosion increase at Beacon Batch, south end headwater at the watershed, Richard Webb 2000 ST4857.

This picture is the basin head of the east tributary depression, winter bracken to the side, exact date uncertain, 1970 is given nearest to flume completion, closest flow record.
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Source From geograph.org.uk
Author MDS
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MDS / Ephemeral Channel / 
MDS / Ephemeral Channel
Camera location51° 18′ 48″ N, 2° 44′ 46″ W  Heading=135° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location51° 18′ 47″ N, 2° 44′ 46″ W  Heading=135° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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current14:50, 30 December 2010Thumbnail for version as of 14:50, 30 December 2010484 × 640 (83 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Ephemeral Channel Pipeflow and interflow combine, with surface runoff between heather ling clumps and peat mounds, to form an ephemeral channel migrating down channel. This moves forward on the drie

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