The Geology of the Carboniferous Limestone, Yoredale Rocks, and Millstone Grit of North Derbyshire: (Parts of Sheets 88 S. E., 81 N. E., 81 S. E., 72 N. E., 82 N. W., 82 S. W., and 71 N. W.)
The Geology of the Carboniferous Limestone, Yoredale Rocks, and Millstone Grit of North Derbyshire: (Parts of Sheets 88 S. E., 81 N. E., 81 S. E., 72 N. E., 82 N. W., 82 S. W., and 71 N. W.)
This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1887 Excerpt: ...nnd about Round Know! west of Stanton; at Greenfield, one mile south-east of Youlgreave, clay with quartz pebbles; at Broad Meadow, one mile east of Youlgreave, clay with many boulders of limestone, very thickly covered with ice-scratches; and by Bury Cliff, three-quarters of a mile north-west of Elton, clay with a few ...
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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1887 Excerpt: ...nnd about Round Know! west of Stanton; at Greenfield, one mile south-east of Youlgreave, clay with quartz pebbles; at Broad Meadow, one mile east of Youlgreave, clay with many boulders of limestone, very thickly covered with ice-scratches; and by Bury Cliff, three-quarters of a mile north-west of Elton, clay with a few limestone pebbles. Traces of what is probably Drift were seen below Peak Tor south of Rowsley, where the soil contained a tew pebbles of limestone and chert. Between Cromford and Bonsall is a rock called the Bloody Stone, which is polished and scratched, possibly by ice. It was noticed by Mr. Mackintosh (Geological Magazine, Vol. II., p. 380), and described by one of the authors of the present Memoir (ibid. p. 440). Sir A. Ramsay has since visited the spot. He declined to give a positive opinion, saying that in a well-glaciated country it would pass muster as a truly ice-scratched rock; but that, lying as it does, the only known evidence for land-glaciation, it was not satisfactory enough to be accepted as conclusive proof. The dip-slope of Riber Hill, south-east of Matlock, is thickly covered with Boulder Clay. Glaciated blocks and pebbles of Mountain Limestone, pieces of chert, and one smoothed and scratched bit of sandstone was seen. The ground is about 350 feet above the bottom of the Derwent valley, but is connected with it by a valley running from Nether Tansley towards Matlock. The country east of Holloway is covered with stiff clay containing many large quartz pebbles. The southern end of the Crich Limestone is covered with Boulder Clay. This ground hes at the head of a broad valley which opens into the valley of the Amber, and is so connected with that of the Derwent. Lastly, over the dip-slope of the Kinder Scout Grit between Alderw...
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All Editions of The Geology of the Carboniferous Limestone, Yoredale Rocks, and Millstone Grit of North Derbyshire: (Parts of Sheets 88 S. E., 81 N. E., 81 S. E., 72 N. E., 82 N. W., 82 S. W., and 71 N. W.)
