9781108072564 - on the geological structure of the alps, apennines and carpathians: more especially to prove a transition from secondary to tertiary rocks, and the ... library collection: earth sciences) von roderick impey murchison (5 Ergebnisse)
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Paperback. Zustand: Very Good. On the Geological Structure of the Alps, Apennines and Carpathians: More Especially to Prove a Transition from Secondary to Tertiary Rocks, and the . Library Collection - Earth Science) This book is in very good condition and will be shipped within 24 hours of ordering. The cover may have some limi…ted signs of wear but the pages are clean, intact and the spine remains undamaged. This book has clearly been well maintained and looked after thus far. Money back guarantee if you are not satisfied. See all our books here, order more than 1 book and get discounted shipping. .
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Zustand: New. Murchison's authoritative study of 1849 which transformed contemporary understanding of European geology. Series: Cambridge Library Collection - Earth Science. Num Pages: 176 pages, 41 b/w illus. BIC Classification: 1DFHA; 1DS; 3JH; RBGD. Category: (P) Professional & Vocational. Dimension: 216 x 140 x 10. Weight in… Grams: 230. . 2011. Reissue. paperback. . . . . Books ship from the US and Ireland.
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Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - Few men were better placed to produce an authoritative study of Continental geology than Roderick Impey Murchison (1792-1871), President of the Geological Society and the Royal Geographical Society of London. Having conducted extensive fieldwork alon…gside Adam Sedgwick, in 1847 Murchison set out on a study tour that would change the manner in which geology was understood and debated. Delivered before the Geological Society and published in their Quarterly Journal in 1849, this paper challenged received wisdom as to the age and formation of the most impressive of geological phenomena. Covering crystalline and palaeozoic rocks, the Trias, iron mines, nummulitic rocks and fish slates, this landmark study and its numerous diagrams that illustrate it not only explain a geological subject, but also reveal the nature of nineteenth-century scientific scholarship. The book also contains a short supplementary paper on the distribution of surface detritus in the Alps.
