Page:The Journal of geology (IA journalofgeology21894univers).pdf/263
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OIL SHALES—SCOTTISH CARBONIFEROUS SYSTEM.
249
Scottish Lothians, the exceeding faulted and disturbed nature of the Carboniferous system in this locality would effectually prevent the circulation underground of any quantity of fluid hydrocarbons except within extremely limited areas.
The following is a general section of the oil shale series west of Edinburgh:
| Feet. | |
|---|---|
| Strata below base of Carboniferous Limestone series about | 400 |
| Raeburns Shale, 3 to 4 feet strata, | 190 |
| Mungals Shale, about 1 ft. 9 ins. strata, | 170 |
| Coal and Gray cypride Shale 2 ft. "Houston Marl" group | 200 |
| Strata laminated sandstones, | 240 |
| Fells Shale, 3 to 5 feet, "Broxburn Marl" group, 80 to | 270 |
| Broxburn Shale 2½ to 8 feet, "Binney Sandstone" and strata, | 450 |
| Dunnet Shale, 6 to 13feet, strata chiefly shales, fire clays, etc. | 400 |
Barracks Shale, resting on the estuarine Burdiehouse Limestone, 10 to 50 feet thick at places, strata about |
780 |
| Pumpherston Shales, about 6 feet worked. | |
| Apparent thickness of Oil shale series, | 3,100 |
Henry M. Cadell.