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- W2326387911 abstract "In carrying out certain geological investigations in Renfrewshire some years ago, I became acquainted with a dolerite bed, crossing the county nearly from south to north, on the east of Paisley, and which is worked as a surface section at Seedhills. Its thickness there is about 22 feet, varying, so far as has been ascertained, from 22 feet to 25 feet. Where not exposed to atmospheric action it is a hard, pure dolerite, splitting with a straight, smooth surface, which makes it very suitable for paving-stones. It is a bed, and not a dyke; the dip being generally to the south-east, and corresponding with that of the adjacent strata; at Seedhills it is 8 degrees.* Its strike, as already mentioned, is usually nearly north and south, with a slight bearing to the east; but still is very irregular, running with ragged edges, sometimes jutting out, as at Seedhills, from 100 to 200 yards to the west, and at other times withdrawing within the main line to the east, as it appears to do north of Arkleston farm-house. At present I have not discovered its true horizon in the Carboniferous strata, but I will put it down, provisionally, above the main limestone and below the clayband ironstone of the Possil series. At one time I was inclined to place it below the main limestone, as I thought that the Blackhall limestone, which lies about 60 feet above it, was an upthrow of the main bed, but further search does not bear This 250-word extract was created in the absence of an abstract" @default.
- W2326387911 created "2016-06-24" @default.
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- W2326387911 date "1877-01-01" @default.
- W2326387911 modified "2023-10-14" @default.
- W2326387911 title "XX. Remarks upon the Bed of Dolerite which crosses Renfrewshire to the east of Paisley" @default.
- W2326387911 doi "https://doi.org/10.1144/transglas.5.2.270" @default.
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