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063-1034 Carboniferous red sandstone beach

XIII.—The Old Red Sandstone Rocks of the West Kilbride-Largs District, Ayrshire

 

EM Patterson

Transactions of the Geological Society of Glasgow 21 (2), 207-236, 1951

From Ardrossan northwards to Wemyss Bay the eastern shores of the Firth of Clyde furnish an almost continuous succession of sandstones, pebbly sandstones and conglomerates referred on the published geological maps to the Upper Old Red Sandstone. These form a foundation for the Carboniferous lava-plateau of Renfrewshire and northern Ayrshire. They rise steeply from the coast towards the lava-country of the interior and separate it from the sea by a distance which varies from half a mile near Largs to upwards of four miles west of the villages of Inverkip and West Kilbride. The district described in the present paper comprises the coastal tract which stretches for a distance of seven miles from West Kilbride to Largs (Fig. 3). It lies mainly within Sheet 21 of the Geological Survey One-inch Map, though a small part on its eastern margin is included in Sheet 22.

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