File:Quartzite outcrop - geograph.org.uk - 901061.jpg

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Summary

Description
English: Quartzite outcrop The cream-coloured, translucent rock outcrops with a very bedded appearance are of the Eriboll Sandstone. These Lower Palaeozoic rocks are exposed in a complex structure known as the Ord Window, formed by folding, faulting and thrusting. The Ord Window shows the most southerly exposures of these rocks which can be found all the way to the North coast of Sutherland.
Date
Source From geograph.org.uk
Author Jonathan Wilkins
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Jonathan Wilkins / Quartzite outcrop / 
Jonathan Wilkins / Quartzite outcrop
Camera location57° 08′ 48″ N, 5° 56′ 40″ W  Heading=112° Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo
Object location57° 08′ 48″ N, 5° 56′ 40″ W  Heading=112° 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: Jonathan Wilkins
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16 July 2008

57°8'47.8"N, 5°56'40.2"W

heading: 112 degree

57°8'47.76"N, 5°56'40.20"W

heading: 112 degree

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current20:23, 21 February 2011Thumbnail for version as of 20:23, 21 February 2011640 × 480 (105 KB)GeographBot== {{int:filedesc}} == {{Information |description={{en|1=Quartzite outcrop The cream-coloured, translucent rock outcrops with a very bedded appearance are of the Eriboll Sandstone. These Lower Palaeozoic rocks are exposed in a complex structure known as t
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