File:Relict solifluction lobe on slopes of Moruisg - geograph.org.uk - 1636311.jpg

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Relict_solifluction_lobe_on_slopes_of_Moruisg_-_geograph.org.uk_-_1636311.jpg(640 × 360 pixels, file size: 86 KB, MIME type: image/jpeg)

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English: Relict solifluction lobe on slopes of Moruisg Mass wasting in periglacial climates in the Pleistocene often gave rise to these lobes of soil and weathered rock. Stones frequently are found fronting the lobes. The reason for the soil flowage is summer melting and therefore lubrication over impermeable permafrost.
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Source From geograph.org.uk
Author Penny Goodman
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Penny Goodman / Relict solifluction lobe on slopes of Moruisg / 
Penny Goodman / Relict solifluction lobe on slopes of Moruisg
Camera location57° 30′ 16″ N, 5° 10′ 36″ W  Heading=180° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location57° 30′ 14″ N, 5° 10′ 36″ W  Heading=180° 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: Penny Goodman
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current17:26, 4 March 2011Thumbnail for version as of 17:26, 4 March 2011640 × 360 (86 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Relict solifluction lobe on slopes of Moruisg Mass wasting in periglacial climates in the Pleistocene often gave rise to these lobes of soil and weathered rock. Stones frequently are found fronting

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