File:Cleit Mòr - geograph.org.uk - 833031.jpg

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Cleit_Mòr_-_geograph.org.uk_-_833031.jpg(640 × 427 pixels, file size: 275 KB, MIME type: image/jpeg)

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English: Cleit Mòr Geologists examining an example of a Scourie dyke cutting across mafic-ultramafic gneisses. The term 'mafic' means that it contains a relatively high proportion of the minerals found in the mantle of the Earth, whereas most crustal rocks are relatively depleted in such minerals. This has implications for the origin of such rocks.
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Source From geograph.org.uk
Author Anne Burgess
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Anne Burgess / Cleit Mòr / 
Anne Burgess / Cleit Mòr
Camera location58° 20′ 47″ N, 5° 10′ 39″ W  Heading=67° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location58° 20′ 47″ N, 5° 10′ 37″ W  Heading=67° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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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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current18:56, 20 February 2011Thumbnail for version as of 18:56, 20 February 2011640 × 427 (275 KB)GeographBot (talk | contribs)== {{int:filedesc}} == {{Information |description={{en|1=Cleit Mòr Geologists examining an example of a Scourie dyke cutting across mafic-ultramafic gneisses. The term 'mafic' means that it contains a relatively high proportion of the minerals found in t

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