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II.—Remarks on the Formation of Landscape Marble
Published online by Cambridge University Press: 01 May 2009
Extract
The Landscape Marble or Cotham Stone is one of the best known of our English ornamental rocks. Polished slabs of it may be seen in most museums; and there are fashioned out of it paperweights, ring-stands, and other useful objects, which may be purchased on Clifton Down and elsewhere.
This stone came into notice when it was quarried, together with other beds, near Cotham House, on the northern side of Bristol; and it was described in considerable detail in 1754 by Edward Owen, who then gave it the name of “Cotham Stone.”
It is a hard, close-grained argillaceous limestone, which breaks with a fracture almost as conchoidal as that of flint; and it is characterized by dark arborescent markings which pervade the stone. These markings rise from a more or less stratified base, and terminate upwards in the wavy banded portion of the limestone, which varies from one to about nine inches in thickness. Thus when slabs, cut at right angles to the planes of bedding, are polished, there may often be discerned (with the aid of the imagination) a landscape with a prominent row of trees and bushes, with clouds above, and perhaps the semblance of water in the foreground.
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References
page 110 note 1 Observations on the Earths, Rocks, Stones, and Minerals, for some miles about Bristol, etc., 8vo. London.
page 110 note 2 An illustration of the Landscape Marble was published in the Proc. Geol. Assoc. vol. i. p. 209.
page 111 note 1 See Dr. Wright, , GEOL. MAG. 1864, p. 291.Google Scholar
page 112 note 1 Geol. Somerset, E., etc. (Geol. Survey), p. 70;Google Scholar and Geol. England and Wales, ed. 2, p. 244.
page 113 note 1 Proc. Geol. Assoc. vol. xi. p. xxx.
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