The geology of England and Wales; a concise account of the lithological characters, leading fossils, and economic products of the rocks with notes on the physical features of the country by Horace Bolingbroke Woodward
The geology of England and Wales; a concise account of the lithological characters, leading fossils, and economic products of the rocks with notes on the physical features of the country by Horace Bolingbroke Woodward PDF, ePub eBook D0wnl0ad
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. 1876 Excerpt: ...100 Middle Chalk with flints, and few fossils.... 400 Chalk Lower Chalk, with few fossils 100 lied and Grey Chalk, with many fossils 40 Red Chalk, Belemnite Listen, &c. 30 He observes that the unconformability of the Chalk to all the strata beneath it is a striking feature of the geology of Yorkshire. The lowest bed of Red Chalk is the equivalent of the Hunstanton Limestone. Mr. Judd has pointed out in regard to the Chalk of Lincolnshire, that the occurrence of the flint layers is very irregular. Above the Chalk Marl is a considerable thickness of hard Chalk (as in Norfolk) which has been used for buildingpurposes. Louth Abbey was in great part constructed of it. Near Louth this series contains a well marked bed of Red Chalk, 5 or 6 feet in thickness, and some other bands of a pinkish hue, all distinct from and much above the Himstan ton limestone. The 'Sponge-bed' with Spongia paradoxica is found at the base of the Chalk series, graduating into the Hunstanton limestone. The Wolds of Lincolnshire are much more covered with superficial deposits than the downs of the south of England, or even Norfolk; hence the district of the Chalk in this county does not present that uniformly bare and arid appearance so characteristic of it in most parts; in fact, nearly the whole of it has now been brought under the plough, and with the most satisfactory results. In Norfolk the Chalk was divided by Mr. Samuel Woodward into:--Upper Chalk, with flints. Medial Chalk, with few flints. Lower or Hard Chalk. Chalk Marl. The thickness of the Chalk-with-flints (Upper and Medial) was proved to be 1,050 feet in a well-boring at Messrs. Colman's at Norwich; and that of the Chalk-without-flints (including the Hard Chalk) 102 feet. The Chalk Marl is only about 3 feet in thickness, ...From reader reviews:
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