P number: | P001982 |
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Old photograph number: | C00116 |
Caption: | View looking west down the Glenmore River from near Cnoc Fhionn, Inverness-shire. |
Description: | The complex consists of a series of rocks that range from minor ultrabasics through the major constituents of diorite, granodiorite, monzonite to adamellite. It belongs to the 'Newer Granites', a series of plutons and smaller igneous intrusions emplaced later than the main metamorphic recrystallization and deformation of the Caledonian Orogeny. The slopes in the foreground are chiefly composed of plutonic rocks belonging to the Glenelg-Ratagain complex. In the middle distance the rocks are Lewisian gneiss and Moine schists. The Skye hills can be seen in the distance. |
Date taken: | Sun Jan 01 00:00:00 GMT 1905 |
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: | 187000 |
Y latitude/northing: | 819000 |
Coordinate reference system, ESPG code: | 27700 (OSGB 1936 / British National Grid) |
Orientation: | Landscape |
Size: | 138.41 KB; 1001 x 728 pixels; 85 x 62 mm (print at 300 DPI); 265 x 193 mm (screen at 96 DPI); |
Average Rating: | Not yet rated |
Categories: | Unsorted Images, Geoscience subjects/ Stratigraphical |
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