| P number: | P000342 |
|---|---|
| Old photograph number: | B00914 |
| Caption: | Achnasheen. Ross & Cromarty. Glaciofluvial terraces. A classic landform site as an example of glaciofluvial outwash and delta terraces formed by meltwater deposition in an ice-dammed lake during the Loch Lomond Stadial c. 11,000-10,000 years ago. |
| Description: | Achnasheen. Ross & Cromarty. Glaciofluvial terraces. A classic landform site as an example of glaciofluvial outwash and delta terraces formed by meltwater deposition in an ice-dammed lake during the Loch Lomond Stadial c. 11,000-10,000 years ago. The large terrace on the left is designated the highest terrace, the railway indicated by the line of telegraph poles runs at its base on a lower terrace. On the right numerous fragments of terraces remain with drift mounds on the upper slopes. The building is the Ledgowan Hotel. |
| Date taken: | Mon Jan 01 00:00:00 GMT 1912 |
| 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: | 215500 |
| Y latitude/northing: | 858500 |
| Coordinate reference system, ESPG code: | 27700 (OSGB 1936 / British National Grid) |
| Orientation: | Landscape |
| Size: | 216.75 KB; 1000 x 758 pixels; 85 x 64 mm (print at 300 DPI); 265 x 201 mm (screen at 96 DPI); |
| Average Rating: | Not yet rated |
| Categories: | Unsorted Images, Geoscience subjects/ Landforms, river/ River terraces and cliffs, Geoscience subjects/ Landforms, glaciation/ Overflow and marginal channels |
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