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Uploaded on:
2009-02-14 03:02:09.0
Type:
Digital Asset
File Size:
225.51 KB
Dimensions:
1001 x 724 pixels
1843 views 4 downloads
P number: P002228
Old photograph number: C02015
Caption: Quinag and Loch Assynt from near Inchnadamph, Sutherland. A mountain of Torridonian sandstone capped by Cambrian Basal Quartzite and resting on an uneven surface that represents an old land surface of Lewisian gneiss.
Description: Quinag and Loch Assynt from near Inchnadamph, Sutherland. A mountain of Torridonian sandstone capped by Cambrian Basal Quartzite and resting on an uneven surface that represents an old land surface of Lewisian gneiss. The mountains in this northern outcrop of the Torridonian sandstone form isolated, characteristic 'inselberg' or 'island mountain' terrain. These sandstones form long narrow ridges separated by broad valleys of Lewisian gneiss. They are a reddish-brown assemblage of terrestrial sedimentary rocks laid down under fluviatile conditions. The rocks on the right are Cambro-Ordovician Durness Group that has undergone thrusting to create an imbricate structure.
Date taken: Thu Jan 01 00:00:00 GMT 1914
Photographer: Lunn, R.
Copyright statement: Crown
Acknowledgment: This image was digitized with grant-in-aid from SCRAN the Scottish Cultural Resources Access Network
X longitude/easting: 220500
Y latitude/northing: 928500
Coordinate reference system, ESPG code: 27700 (OSGB 1936 / British National Grid)
Orientation: Landscape
Size: 225.51 KB; 1001 x 724 pixels; 85 x 61 mm (print at 300 DPI); 265 x 192 mm (screen at 96 DPI);
Average Rating: Not yet rated
Categories: Unsorted Images, Geoscience subjects/ Igneous features/ Volcanic vents, necks and plugs  

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