| P number: | P001905 |
|---|---|
| Old photograph number: | C01309 |
| Caption: | 2.4 km. west of Ardchuilk, Glen Strathfarrar, Inverness-shire. In middle distance - two glacial dry valleys on north side of River Farrar. On left are remnants of a fluvioglacial terrace. Silted-up lake basin in the foreground. |
| Description: | 2.4 km. west of Ardchuilk, Glen Strathfarrar, Inverness-shire. In middle distance - two glacial dry valleys on north side of River Farrar. On left are remnants of a fluvioglacial terrace. Silted-up lake basin in the foreground. East end of postglacial lake in foreground (see photos C01310, C01311). Low terrace of glaciofluvial deposits in left foreground to middle ground, crossed by road. Rock bar damming lake in middle distance (just above road) has two notches, possibly overflow channels when present exit to lake basin was still blocked by ice. Bedrock is mostly psammite (metamorphosed sandstone), with units of pelite (metamorphosed mudstone), here commonly garnetiferous and gneissose, up to 0.5 km. wide. All these rocks belong to the Moine Supergroup (probably Glenfinnan Group). |
| Date taken: | Sat Jan 01 00:00:00 GMT 1910 |
| 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: | 224500 |
| Y latitude/northing: | 838500 |
| Coordinate reference system, ESPG code: | 27700 (OSGB 1936 / British National Grid) |
| Orientation: | Landscape |
| Size: | 222.92 KB; 1000 x 719 pixels; 85 x 61 mm (print at 300 DPI); 265 x 190 mm (screen at 96 DPI); |
| Average Rating: | Not yet rated |
| Categories: | Unsorted Images |
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