File:Blorenge looms behind Llanfoist's moraine-by-Alan-Bowring.jpg

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English: Much of Llanfoist is built on the Llanfoist-Nevil Hall moraine, deposited by a receding Usk valley glacier during the last ice age. The wooded pool in the foreground does not appear on Ordnance Survey maps yet is an enduring feature, filling a large hollow in the moraine. Cwm Craf on the front face of Blorenge beyond is likely to be a nivation hollow rather than a glacial cirque.
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Source From geograph.org.uk
Author Alan Bowring
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Creative Commons Attribution Share-alike license 2.0
Camera location51° 48′ 45.02″ N, 3° 01′ 31.84″ W  Heading=225° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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attribution share alike
This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: Alan Bowring
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Date/TimeThumbnailDimensionsUserComment
current21:29, 18 September 2017Thumbnail for version as of 21:29, 18 September 20172,816 × 2,112 (2.5 MB)Geograph Update Bot (talk | contribs)Higher-resolution version from Geograph.
14:02, 14 September 2014Thumbnail for version as of 14:02, 14 September 2014640 × 480 (89 KB)Bikeroo (talk | contribs)User created page with UploadWizard

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