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Home > An Elementary Treatise on Mineralogy and Geology (Volume 2); Designed for the Use of Pupils for Persons, Attending Lectures on These Subjects and as a Companion for Travellers in the United States of America: (English)
An Elementary Treatise on Mineralogy and Geology (Volume 2); Designed for the Use of Pupils for Persons, Attending Lectures on These Subjects and as a Companion for Travellers in the United States of America: (English)

An Elementary Treatise on Mineralogy and Geology (Volume 2); Designed for the Use of Pupils for Persons, Attending Lectures on These Subjects and as a Companion for Travellers in the United States of America: (English)

          
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About the Book

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. 1822. Excerpt: ... few in number. In stratified minerals there is, in general, a remarkably distinct and sudden transition from one stratum to another; and, in many cases, contiguous strata are totally unlike each other. Thus beds of shale, sandstone, limestone, coal, clay, &c. alternate with each other, and, in some cases, several times in succession, indeed soft strata of clay are sometimes found under beds of limestone, &c. and loose sand is sometimes interposed between indurated strata. It is sufficient to ask, could these facts exist, if minerals had been formed by the fusion of heterogeneous masses of sand and gravel, or consolidated by the injection of melted matter among loose grains of different substances promiscuously. mingled? Could, for example, certain varieties of anthracite lose their bitumen by heat, and yet retain their pyrites, composed in part of sulphur?--On the contrary, the facts just stated would probably result from the formation of minerals in an aqueous fluid. Sect. 4. Veins. 37. All veins appear to have once been open fissures, which have subsequently been filled by substances, that are usually more or less different from the surrounding rock.--In some cases, they have been filled by successive deposites of different minerals. Sometimes indeed only one mineral is present; but, most frequently, several substances occur in the same vein. Many of the saline and earthy minerals, most of the ores, and some aggregates more or less frequently occur in veins. 38. Veins, though sometimes parallel to the direction of the strata, more frequently traverse it, and may thus be distinguished from beds, which are always parallel to the contiguous strata. It has been remarked, that those veins, which occur in the vicinity of each other and contain the same minera...


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Product Details
  • ISBN-13: 9781154225792
  • Publisher: General Books
  • Publisher Imprint: General Books
  • Height: 246 mm
  • No of Pages: 364
  • Series Title: English
  • Weight: 649 gr
  • ISBN-10: 1154225798
  • Publisher Date: 30 Jan 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Spine Width: 19 mm
  • Width: 189 mm


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An Elementary Treatise on Mineralogy and Geology (Volume 2); Designed for the Use of Pupils for Persons, Attending Lectures on These Subjects and as a Companion for Travellers in the United States of America: (English)
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An Elementary Treatise on Mineralogy and Geology (Volume 2); Designed for the Use of Pupils for Persons, Attending Lectures on These Subjects and as a Companion for Travellers in the United States of America: (English)
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