P number: | P002694 |
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Old photograph number: | D01071 |
Caption: | Garleton Hills, Craigy Hill, East Lothian. |
Description: | Garleton Hills, Craigy Hill, East Lothian. Lower Carboniferous trachyte lava flow at the top of the Garleton Hills Volcanic Formation, Strathclyde Group. The rock is commonly rotted and well jointed and tends to weather into small fragments. These fall to the base of the cliff forming the scree slope below, as seen in the photograph. The Midland Valley of Scotland was quite active volcanically during the early Carboniferous period, with huge volumes of lava erupted. In the western part of the Midland Valley this was almost wholly basaltic in composition whereas in the east, some trachytic flows occur, especially in the area north and east of Haddington. |
Date taken: | Sun Jan 01 00:00:00 GMT 1967 |
Photographer: | Christie, A. |
Copyright statement: | NERC |
Acknowledgment: | This image was digitized with grant-in-aid from SCRAN the Scottish Cultural Resources Access Network |
X longitude/easting: | 351100 |
Y latitude/northing: | 676500 |
Coordinate reference system, ESPG code: | 27700 (OSGB 1936 / British National Grid) |
Orientation: | Landscape |
Size: | 187.27 KB; 1001 x 777 pixels; 85 x 66 mm (print at 300 DPI); 265 x 206 mm (screen at 96 DPI); |
Average Rating: | Not yet rated |
Categories: | Unsorted Images |
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