File:A Scourie Dyke - geograph.org.uk - 833049.jpg
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[edit]DescriptionA Scourie Dyke - geograph.org.uk - 833049.jpg |
English: A Scourie Dyke The line of dark rock cutting through the paler gneiss is a Scourie dyke. Scourie dykes were intruded between 2400 and 2200 million years ago into the Lewisian gneiss, which is at least 2700 million years old. This is a very narrow dyke, but they can be up to tens of metres in width. Notice how sharp the contact between the dyke and the country rock is. |
Date | |
Source | From geograph.org.uk |
Author | Anne Burgess |
Attribution (required by the license) InfoField | Anne Burgess / A Scourie Dyke / |
InfoField | Anne Burgess / A Scourie Dyke |
Camera location | 58° 20′ 47.9″ N, 5° 10′ 39″ W | View this and other nearby images on: OpenStreetMap | 58.346640; -5.177500 |
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Object location | 58° 20′ 47.9″ N, 5° 10′ 39″ W | View this and other nearby images on: OpenStreetMap | 58.346640; -5.177500 |
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Licensing
[edit]This image was taken from the Geograph project collection. See this photograph's page on the Geograph website for the photographer's contact details. The copyright on this image is owned by Anne Burgess and is licensed for reuse under the Creative Commons Attribution-ShareAlike 2.0 license.
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This file is licensed under the Creative Commons Attribution-Share Alike 2.0 Generic license.
Attribution: Anne Burgess
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current | 18:29, 20 February 2011 | 507 × 640 (346 KB) | GeographBot (talk | contribs) | == {{int:filedesc}} == {{Information |description={{en|1=A Scourie Dyke The line of dark rock cutting through the paler gneiss is a Scourie dyke. Scourie dykes were intruded between 2400 and 2200 million years ago into the Lewisian gneiss, which is at lea |
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