This scarce antiquarian book is a facsimile reprint of the original. Due to its age, it may contain imperfections such as marks, notations, marginalia and flawed pages. Because we believe this work is culturally important, we have made it available as part of our commitment for protecting, preserving, and promoting the world's literature in affordable, high quality, modern editions that are true to the original work.
Die Inhaltsangabe kann sich auf eine andere Ausgabe dieses Titels beziehen.
This scarce antiquarian book is a facsimile reprint of the original. Due to its age, it may contain imperfections such as marks, notations, marginalia and flawed pages. Because we believe this work is culturally important, we have made it available as part of our commitment for protecting, preserving, and promoting the world's literature in affordable, high quality, modern editions that are true to the original work.
British area has passed. The pioneer in this branch of geological science wasM r, Godwin-A usten, whose masterly essays published in the Quarterly Journal of the Geological Society, between 1856 and 1866, may still be read with advantage, for many of his conclusions have been confirmed by the information subsequently derived from deep borings in the eastern and midland counties. Many geologists have dealt in more or less detail with the geographical conditions of particular epochs, but the first systematic treatise on the geography of successive geological periods was that by Professor Hull, published in 1882, and entitled, Contributions to the Physical History of theB ritish I sles. The larger part of Professor Hull sbook, however, is devoted to the consideration of the Palaeozoic periods and the origin of the Atlantic Ocean; the space allotted to theN eozoic periods being hardly proportionate to the knowledge that we really possess concerning them. The aim and scope of the present volume are somewhat different from Professor Hull s, the successive periods of Neozoic time being treated at much greater length than those of Palaeozoic time, partly because much more information is available, but chiefly because it is my object to trace out the succession of physical and geographical changes which have led up to the existing disposition of land and water in the north-western portion of Europe. My thanks are due to many friends and correspondents for information and advice, especially toD r. Callaway with regard to the Cambrian period, toP rofessor Hull respecting the I rish Devonians, toP rofessor A. H. Green, Mr. E. Wilson, and Mr. H. B.
(Typographical errors above are due to OCR software and don't occur in the book.)
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Taschenbuch. Zustand: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - This scarce antiquarian book is a facsimile reprint of the original. Due to its age, it may contain imperfections such as marks, notations, marginalia and flawed pages. Because we believe this work is culturally important, we have made it available as part of our commitment for protecting, preserving, and promoting the world's literature in affordable, high quality, modern editions that are true to the original work. Bestandsnummer des Verkäufers 9780548587317
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