File:Glacial overflow channel near Kilburn - geograph.org.uk - 683045.jpg

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Glacial_overflow_channel_near_Kilburn_-_geograph.org.uk_-_683045.jpg(640 × 480 pixels, file size: 74 KB, MIME type: image/jpeg)

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English: Glacial overflow channel near Kilburn The west and south sides of the Hambleton Hills have a number of these valleys, channels or gaps along the base of the scarp. They appear to have been formed by meltwaters draining off the hilltops and then being forced around the margin of the slowly decaying glacier in the Vales of Mowbray and York. Most are now dry, or contain small lakes such as this one.
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Source From geograph.org.uk
Author Gordon Hatton
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Gordon Hatton / Glacial overflow channel near Kilburn / 
Gordon Hatton / Glacial overflow channel near Kilburn
Camera location54° 12′ 57″ N, 1° 13′ 56″ W  Heading=67° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location54° 12′ 58″ N, 1° 13′ 51″ W  Heading=67° 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: Gordon Hatton
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current01:41, 8 February 2011Thumbnail for version as of 01:41, 8 February 2011640 × 480 (74 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Glacial overflow channel near Kilburn The west and south sides of the Hambleton Hills have a number of these valleys, channels or gaps along the base of the scarp. They appear to have been formed by

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