The Carboniferous System in Scotland Characterized by its Brachiopoda
“This group in Northumberland is seen, westward of Alnwick at Garmitage-bank and Crawley Dean, and on the flanks of the porphyry of the Cheviot in Biddleston Burn, and in the Coquet below Linn Brig; it occupies a considerable area in the south part of Berwickshire, and is largely developed on the Tweed at Carham, Coldstream, Norham, etc.; it is seen underlying the mountain-limestone on the sea-coast from near Lammerton Shiel to Burnmouth; on the north side of Lammermuirs it is intercalated between the Old Red Sandstone, and the mountain-limestone from the Pees mouth to the Cove harbour.” Mr. Tate observes also that the Campsie and Fifeshire beds resemble those of Northumberland.
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1906 ◽
Vol 12
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pp. 415-430
Keyword(s):
1789 ◽
Vol 79
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pp. 65-70
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1832 ◽
Vol 1
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pp. 230-232
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1917 ◽
Vol 7
(2)
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pp. 51-60
Keyword(s):
1953 ◽
Vol 48
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pp. 19-29
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Keyword(s):
1916 ◽
Vol 2
(2)
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pp. 194-209