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Geological Sketches at Home and Abroad (1882) by Archibald Geikie

Geological Sketches at Home and Abroad (1882)

Archibald Geikie
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Details

  • ISBN
    9780217480642 / 0217480640
  • Title Geological Sketches at Home and Abroad (1882)
  • Author Archibald Geikie
  • Format
    Paperback
  • Year 2010
  • Pages 92
  • Publisher
    Rarebooksclub.com
  • Imprint Rarebooksclub.com
  • Language English
  • Dimensions 152mm x 11mm x 229mm

Annotation

This is an OCR edition without illustrations or index. It may have numerous typos or missing text. However, purchasers can download a free scanned copy of the original rare book from GeneralBooksClub.com. You can also preview excerpts from the book there. Purchasers are also entitled to a free trial membership in the General Books Club where they can select from more than a million books without charge. Original Published by: Macmillan in 1882 in 404 pages; Subjects: Geology; Juvenile Nonfiction / Science & Nature / Earth Sciences / General; Science / General; Science / Earth Sciences / General; Science / Earth Sciences / Geology;

Publisher Description

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. 1882 edition. Excerpt: ...moisture. When this interstitial water is frozen, its expansive force, as it passes into the solid state, must increase the isolation of the granules and augment the dimensions of a marble block. I am inclined to believe that this must be the principal cause of the change. Whatever may be the nature of the process it is evidently one which acts from within the marble itself. Microscopic examination fails to discover any chemical transformation which would account for the expansion. Dr. Angus Smith has pointed out that in towns the mortar of walls may be observed to swell up and lose cohesion from a conversion of its lime into the condition of sulphate. I have already mentioned that sulphate does exist within the substance of the marble, but that its quantity, so far as I have observed, is too small to be taken into account in this question. The expansive power is exerted in such a way as not sensibly to affect the internal structure and composition of the stone. And this I imagine is most probably the work of frost. The results of my observations among our burial-grounds show that, save in exceptionally sheltered situations, slabs of marble, exposed to the weather in such a climate and atmosphere as that of Edinburgh, are entirely destroyed in less than a century. Where this destruction takes place by simple comparatively rapid superficial solution and removal of the stone, the rate of lowering of the surface amounts sometimes to about a third of an inch (or roughly 9 millimetres) in a century. Where it is effected by internal displacement, a curvature of 2 inches, with abundant rents, a partial effacement of the inscription, and a reduction of the marble to a pulverulent condition, may be produced in about forty years, and a total disruption and...

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Geological Sketches at Home and Abroad (1882)

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