File:Fossil Tree - geograph.org.uk - 801771.jpg

Fossil_Tree_-_geograph.org.uk_-_801771.jpg(640 × 480 pixels, file size: 109 KB, MIME type: image/jpeg)

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English: Fossil Tree Unlike most wood fossils this has not been created by petrification. It is more likely caused when the area became submerged millions of years ago and sediment covered the tree base. Water would have gradually seeped in and the minerals it contained eventually replaced the wood to form the fossil. It has the same shape as the original stump, but chemically is more similar to rock.
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Source From geograph.org.uk
Author Karen Vernon
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Karen Vernon / Fossil Tree / 
Karen Vernon / Fossil Tree
Camera location56° 15′ 20″ N, 2° 37′ 40″ W  Heading=202° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location56° 15′ 19″ N, 2° 37′ 40″ W  Heading=202° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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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: Karen Vernon
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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current08:22, 20 February 2011Thumbnail for version as of 08:22, 20 February 2011640 × 480 (109 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Fossil Tree Unlike most wood fossils this has not been created by petrification. It is more likely caused when the area became submerged millions of years ago and sediment covered the tree base. Wat

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