Annals of the Lyceum of Natural History of New York (Volume 8)

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Published by University of Michigan Library
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Title: Annals of the Lyceum of Natural History of ...
Publisher: University of Michigan Library


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Lyceum of Natural History (New York, N.
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N y Lyceum of Natural History (New York
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Lyceum Of Natural History
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Book Description Rarebooksclub.com, United States, 2012. Paperback. Book Condition: New. 246 x 189 mm. Language: English . Brand New Book ***** Print on Demand *****. 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. 1867 Excerpt: .been observed. The upper surface of certain beds consists of a thin layer or scale of limestone differing from the preceding. Its color is usually light to dark brown. Fracture even. Specific gravity =2.67. It is always very fine-grained and compact, sometimes massive, but often displays on its vertical section, a series of fine horizontal lines of lamination. It is evidently a deposit of an impure carbonate of lime from at least partial solution in water; and as it occurs in layers intervening between the beds, thus marking their stratification, its section (which is always quite distinct in contrast with the white limestones) may be styled the bedding-line. It always adheres to the bed on which it lies, and is partially incorporated with it. A few series of specific gravity determinations have been made upon specimens of the limestone of each bed, selected on the same vertical lines at different heights on the sides of quarries. In all these determinations the specimens were coarsely pulverized, and distilled water at 80 F. employed. The upward increase of the density of the material of each bed is thus displayed, except in bed A, in which Calc Spar occurs in the fossils. 8. Modes of Fossilization.--In these beds there are five modes by which the fossil organism is represented. First, The original shell (or its thickest portion) remains, retaining all its physical and chemical characteristics. No corals are thus preserved. Secondly, The organic matter has decomposed and been removed, but the inorganic remains as a smootli white mass, retaining the form and markings of the original shell, very soft to the touch and friable. Specimens of Porites are also frequently thus preserved. Thirdly, In corals and the larger shells, the cavity between the casts. Bookseller Inventory # APC9781235990052

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Lyceum of Natural History
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Book Description RareBooksClub. Paperback. Book Condition: New. This item is printed on demand. Paperback. 142 pages. Dimensions: 9.7in. x 7.4in. x 0.3in.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. 1867 Excerpt: . . . been observed. The upper surface of certain beds consists of a thin layer or scale of limestone differing from the preceding. Its color is usually light to dark brown. Fracture even. Specific gravity 2. 67. It is always very fine-grained and compact, sometimes massive, but often displays on its vertical section, a series of fine horizontal lines of lamination. It is evidently a deposit of an impure carbonate of lime from at least partial solution in water; and as it occurs in layers intervening between the beds, thus marking their stratification, its section (which is always quite distinct in contrast with the white limestones) may be styled the bedding-line. It always adheres to the bed on which it lies, and is partially incorporated with it. A few series of specific gravity determinations have been made upon specimens of the limestone of each bed, selected on the same vertical lines at different heights on the sides of quarries. In all these determinations the specimens were coarsely pulverized, and distilled water at 80 F. employed. The upward increase of the density of the material of each bed is thus displayed, except in bed A, in which Calc Spar occurs in the fossils. 8. Modes of Fossilization. --In these beds there are five modes by which the fossil organism is represented. First, The original shell (or its thickest portion) remains, retaining all its physical and chemical characteristics. No corals are thus preserved. Secondly, The organic matter has decomposed and been removed, but the inorganic remains as a smootli white mass, retaining the form and markings of the original shell, very soft to the touch and friable. Specimens of Porites are also frequently thus preserved. Thirdly, In corals and the larger shells, the cavity between the casts. . . This item ships from La Vergne,TN. Paperback. Bookseller Inventory # 9781235990052

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Lyceum of Natural History (New York
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Lyceum Of Natural History (New York, N.Y
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Lyceum of Natural History (New York
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Lyceum Of Natural History (New York, N.Y
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Lyceum of Natural History (New York, N.Y
Published by Arkose Press (2016)
ISBN 10: 1346070075 ISBN 13: 9781346070070
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Book Description Arkose Press, 2016. Paperback. Book Condition: New. PRINT ON DEMAND Book; New; Publication Year 2016; Not Signed; Fast Shipping from the UK. No. book. Bookseller Inventory # ria9781346070070_lsuk

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