File:The almost pencil-thin waterfall of Blowing Gill Dyke - geograph.org.uk - 650890.jpg

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English: The almost pencil-thin waterfall of Blowing Gill Dyke The reason for the tiny misfit stream of Blowing Gill Dyke cascading into a clearly much larger gritstone amphitheatre is that its headwaters have been captured more recently by East Gill Dyke to the south, as evident on the 1:25000 map.
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Source From geograph.org.uk
Author Mick Borroff
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Mick Borroff / The almost pencil-thin waterfall of Blowing Gill Dyke / 
Mick Borroff / The almost pencil-thin waterfall of Blowing Gill Dyke
Camera location54° 09′ 43.07″ N, 1° 57′ 05.1″ W  Heading=225° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location54° 09′ 42.2″ N, 1° 57′ 06.6″ W  Heading=225° 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: Mick Borroff
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current16:26, 7 February 2011Thumbnail for version as of 16:26, 7 February 2011640 × 480 (102 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=The almost pencil-thin waterfall of Blowing Gill Dyke The reason for the tiny misfit stream of Blowing Gill Dyke cascading into a clearly much larger gritstone amphitheatre is that its headwaters ha

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