P number: | P000355 |
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Old photograph number: | C01347 |
Caption: | Gleann Einich, 9.7 km. south-south-east of Aviemore. Inverness-shire. Deltaic fluvioglacial terraces of sand and gravel isolated and denuded by subsequent stream action. |
Description: | Gleann Einich, 9.7 km. south-south-east of Aviemore. Inverness-shire. Deltaic fluvioglacial terraces of sand and gravel isolated and denuded by subsequent stream action. Sections through the deposits indicate finely laminated sandy clays with intercalations of sand and fine gravel. The material becomes coarse as it passes upwards and it is capped with several feet of coarse but well-rounded gravel with large boulders. The overall picture in the area was one where the high northern slopes of the Cairngorms were mostly free of ice, apart from the high corrie hanging glaciers. The great hollow of Glen More was filled with an ice mass, tongues of which protruded into the lower parts of Gleann Einich and the Lairig Ghru forming a dam behind which a glacial lake formed. |
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: | 292500 |
Y latitude/northing: | 803500 |
Coordinate reference system, ESPG code: | 27700 (OSGB 1936 / British National Grid) |
Orientation: | Landscape |
Size: | 184.68 KB; 1000 x 731 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/ Landforms, river/ River terraces and cliffs |
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