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- W2074359969 abstract "In this paper I shall first refer to a series of arenaceous and calcareous shales which lie between the Old Red Conglomerate and Lower Limestone Shales, and which represent the true basis of the Carboniferous rocks in Gloucestershire. (2) I shall refer to some beds in the Lower Limestone Shales which may serve as horizons for correlation with other coalfields. (3) I shall consider some features in the Millstone Grit. 1.The Old Red Conglomerate at Dry brook dips to the south-east at an angle of 38°. It is made up of “vein-stone” quartz pebbles, grains of ordinary quartz, measuring about ·021 of an inch in diameter, plates of mica, and a little felspar. Of the quartz grains about fourteen per cent. can be recognized as crystals; but the rest are waterworn. The grains are coated with oxide of iron; but on this being removed by acid, cavities are exposed to view, some of which contain bubbles. In addition to the deposition of oxide of iron on the grains, silica is often found attached to them in minute well-defined and clear crystals.The Old Red Conglomerate passes conformably into a series of loose sandy beds and light and greenish-coloured calcareous shales, dark shales being absent. A section of these beds, carefully measured by the late Mr. John Jones and Mr. W. C. Lucy, F.G.S., showing 247 feet and 108 divisions, appeared in the Proceedings of the Cotteswold Club for 1867. They are there termed “Transition Beds.” Sir H. de la Beche" @default.
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- W2074359969 date "1883-02-01" @default.
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- W2074359969 title "On the Lower Carboniferous Rocks of the Forest of Dean, as represented in Typical Sections at Drybrook" @default.
- W2074359969 doi "https://doi.org/10.1144/gsl.jgs.1883.039.01-04.16" @default.
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