File:Cefn y Galchen - geograph.org.uk - 492257.jpg

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Cefn_y_Galchen_-_geograph.org.uk_-_492257.jpg (640 × 459 pixels, file size: 68 KB, MIME type: image/jpeg)

Captions

Captions

Cefn y Galchen

Summary

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Description
English: Cefn y Galchen Weathered quartzite outcrops near the car park. Looking towards Blorenge. These blocks were formed by intense frost-shattering processes at the end of the last ice age leaving only a few isolated blocks upstanding. The blocks have been rounded at the edges due to less intense but continuous weathering over the last 9,000 years.
Date
Source From geograph.org.uk
Author David Luther Thomas
Attribution
(required by the license)
InfoField
David Luther Thomas / Cefn y Galchen / 
David Luther Thomas / Cefn y Galchen
Camera location51° 47′ 26″ N, 3° 04′ 10″ W  Heading=22° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location51° 47′ 26″ N, 3° 04′ 10″ W  Heading=22° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

Licensing

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w:en:Creative Commons
attribution share alike
This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: David Luther Thomas
You are free:
  • to share – to copy, distribute and transmit the work
  • to remix – to adapt the work
Under the following conditions:
  • attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
  • share alike – If you remix, transform, or build upon the material, you must distribute your contributions under the same or compatible license as the original.

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Date/TimeThumbnailDimensionsUserComment
current04:32, 5 February 2011Thumbnail for version as of 04:32, 5 February 2011640 × 459 (68 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Cefn y Galchen Weathered quartzite outcrops near the car park. Looking towards Blorenge. These blocks were formed by intense frost-shattering processes at the end of the last ice age leaving only

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