File:Carreg Lwyd - geograph.org.uk - 416492.jpg

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Carreg_Lwyd_-_geograph.org.uk_-_416492.jpg (640 × 480 pixels, file size: 95 KB, MIME type: image/jpeg)

Captions

Captions

Carreg Lwyd

Summary

[edit]
Description
English: Carreg Lwyd Carreg Lwyd has a fractured shelf of exposed rock that runs all around its north top. This is the view from one prominence to another. The rock strata in this area are unusually level, so the flattish top of the mountains here have large sections of slabs for a floor.
Date
Source From geograph.org.uk
Author Nigel Davies
Attribution
(required by the license)
InfoField
Nigel Davies / Carreg Lwyd / 
Nigel Davies / Carreg Lwyd
Camera location51° 49′ 25″ N, 3° 38′ 55″ W  Heading=247° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location51° 49′ 22″ N, 3° 39′ 14″ W  Heading=247° 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: Nigel Davies
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.

File history

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Date/TimeThumbnailDimensionsUserComment
current00:35, 4 February 2011Thumbnail for version as of 00:35, 4 February 2011640 × 480 (95 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Carreg Lwyd Carreg Lwyd has a fractured shelf of exposed rock that runs all around its north top. This is the view from one prominence to another. The rock strata in this area are unusually level, s

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