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- W2017443096 abstract "In working the coal-seams of Lancashire, particularly in those seams found near the Gannister mine, from time to time isolated boulders have been discovered, the position of which it is not easy to explain. These boulders are not always of the same kind. They generally consist of granite, quartz, or quartzite, and probably of local rocks which do not particularly attract the attention of the workmen in the collieries. They vary in size from an inch to six or eight inches in diameter, the largest being of granite. A fine specimen has lately been found at Old Meadows Pit, near Bacup, Lancashire, by Mr. John Lord, Bacup. It weighs 6 lb. The granite is composed of quartz, reddish felspar, and hornblende. This boulder was imbedded in the chief coal of the Rossendale district, the Gannister or Mountain Mine, at a distance of 180 ft. from the surface of the ground. Between this seam and the surface, besides sandstones and shales, are found the Upper Foot or Bullion Coal, the Forty Yards9 Mine, and a small Cannel Coal, as seen in the accompanying section:— There was no trace of disturbance in the strata near where the boulder was found. Similar boulders have been found at Crawshawbooth and Goodshaw Hill, about four miles from Burnley, at, Wholaw Nook and Burnt Hills Coalpits, in the same district, and at Higher Dog Hill, Oldham. They are also said to occur in the neighbourhood of Leeds. The boulders in every case are isolated. Sometimes they" @default.
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- W2017443096 date "1887-02-01" @default.
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- W2017443096 title "On Boulders found in Seams of Coal" @default.
- W2017443096 doi "https://doi.org/10.1144/gsl.jgs.1887.043.01-04.55" @default.
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