...The Geology of Coal And Coal-Mining
...The Geology of Coal And Coal-Mining
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16. THE COALFIELDS OF SCOTLAND. Lands and stretching from the Firth of Clyde to the Firth of Forth. Numerous coal-seams occur in the Lower as well as in the Upper Carboniferous Series, COALFIELDS OF GREAT BRITAIN 221 more than one-quarter of the coal still remaining to be worked lying in the Carboniferous Limestone Series. The original area over which the Carboniferous strata were deposited lies between the Ochil and Lennox Hills on the north, and the Lammermuir and Southern Uplands of Ayrshire... on the south. Owing to earth-movements in operation during the Carboni- ferous period, the sediments were deposited in an irregular manner, and it is a matter of speculation as to what extent these separate coal-basins were originally connected, and how much of their present isolation has been brought about by post-Carboniferous folding and denudation. It is, however, usually considered that the Upper and Lower Carboniferous strata once con- tinuously covered an area of 3, 600 square miles, which has been reduced by subsequent denudation to about 1, 680 square miles.
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To quickly assess the difficulty of the text, read a short excerpt:
16. THE COALFIELDS OF SCOTLAND. Lands and stretching from the Firth of Clyde to the Firth of Forth. Numerous coal-seams occur in the Lower as well as in the Upper Carboniferous Series, COALFIELDS OF GREAT BRITAIN 221 more than one-quarter of the coal still remaining to be worked lying in the Carboniferous Limestone Series. The original area over which the Carboniferous strata were deposited lies between the Ochil and Lennox Hills on the north, and the Lammermuir and Southern Uplands of Ayrshire... on the south. Owing to earth-movements in operation during the Carboni- ferous period, the sediments were deposited in an irregular manner, and it is a matter of speculation as to what extent these separate coal-basins were originally connected, and how much of their present isolation has been brought about by post-Carboniferous folding and denudation. It is, however, usually considered that the Upper and Lower Carboniferous strata once con- tinuously covered an area of 3, 600 square miles, which has been reduced by subsequent denudation to about 1, 680 square miles.
What to read after ...The Geology of Coal And Coal-Mining?
You can find similar books in the "Read Also" column, or choose other free books by Walcot Gibson to read onlineMoreLess
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