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Author: Thomas Sterry Hunt
Publisher: Forgotten Books
ISBN: 9781527970694
Category : Science
Languages : en
Pages : 734
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Book Description
Excerpt from Mineral Physiology and Physiography Intimately connected with this subject, and at the same time bearing directly upon the different hypotheses touch ing the genesis of crystalline rocks, is the history of the serpentines, which have been alternately regarded as igneous and as' aqueous, as exotic and as indigenous masses, and in either case were supposed to have been the subject of various metasomatic changes. In the tenth essay, the origimand the geognostic relations of these rocks, as found alike among eozoic and paleozoic strata, are considered, and in this connection the history of many crystalline eozoic groups on both continents, but espe cially in central and southern Europe, has been reviewed, - thus continuing the subject begun in the preceding essay. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
Author: Thomas Sterry Hunt
Publisher: Forgotten Books
ISBN: 9781527970694
Category : Science
Languages : en
Pages : 734
Get Book Here
Book Description
Excerpt from Mineral Physiology and Physiography Intimately connected with this subject, and at the same time bearing directly upon the different hypotheses touch ing the genesis of crystalline rocks, is the history of the serpentines, which have been alternately regarded as igneous and as' aqueous, as exotic and as indigenous masses, and in either case were supposed to have been the subject of various metasomatic changes. In the tenth essay, the origimand the geognostic relations of these rocks, as found alike among eozoic and paleozoic strata, are considered, and in this connection the history of many crystalline eozoic groups on both continents, but espe cially in central and southern Europe, has been reviewed, - thus continuing the subject begun in the preceding essay. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
Author: Thomas Sterry Hunt
Publisher:
ISBN:
Category : Chemistry
Languages : en
Pages : 744
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Author: Thomas Sterry Hunt
Publisher: Theclassics.Us
ISBN: 9781230205366
Category :
Languages : en
Pages : 238
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Book Description
This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1886 edition. Excerpt: ... 10,000 feet or more of diversified and folded Cambrian strata is exchanged in the Adirondack and Mississippi areas for a far more simple type of horizontal strata, but a few hundred feet in thickness; and, secondly, that erosion has removed this great series wholly or in part from over large portions of its original area. 141. With these explanations before us, we are now prepared to consider the relations of the Cambrian and Ordovician series, in their two unlike types of the Appalachian and Adirondack areas, to the Lower Taconic limestones. It has already been shown that Emmons, in 1842, in his final report on the geology of the Northern district of New York, defined, with the present names, the lower subdivisions of the New York paleozoic system, from the Potsdam to the Oneida sandstone, both inclusive, to which he gave the collective appellation of the Champlain division. He at the same time proposed for the Primitive Quartz-rock, the Primitive Lime-rock, and the Transition Argillite of Eaton, together with the First or Transition Graywacke--called by Emmons the Taconic slates--and the Sparry Lime-rock of Eaton, the general name of the Taconic system. The Taconic slates were then described by him as a great mass of argillites with interbedded limestones and coarse sandstones, limited on the east, in his original section, by the Sparry Lime-rock at the base of the Taconic hills, and on the west by "the Loraine or Hudson-River shales," by which the Taconic slates were declared to be undoubtedly overlapped, although the line of junction on the west was said to be obscure. This intermediate mass, whose limits were thus clearly defined to the west of the Taconic hills in 1842, was farther said in 1846 to have an immense thickness, ...
Author: T. S. Hunt
Publisher:
ISBN:
Category :
Languages : en
Pages : 0
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Author: Thomas Sterry Hunt
Publisher:
ISBN: 9783337638535
Category :
Languages : en
Pages : 736
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Author: Thomas Sterry Hunt
Publisher: Scholar's Choice
ISBN: 9781298412591
Category :
Languages : en
Pages : 734
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Book Description
This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it. This work was reproduced from the original artifact, and remains as true to the original work as possible. Therefore, you will see the original copyright references, library stamps (as most of these works have been housed in our most important libraries around the world), and other notations in the work. This work is in the public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work.As a reproduction of a historical artifact, this work may contain missing or blurred pages, poor pictures, errant marks, etc. Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.
Author: Thomas Sterry Hunt
Publisher:
ISBN:
Category : Crystalline rocks
Languages : en
Pages : 710
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Author: Thomas Sterry Hunt
Publisher:
ISBN:
Category :
Languages : en
Pages : 710
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Author: Thomas Sterry Hunt
Publisher:
ISBN:
Category : Geologists
Languages : en
Pages : 46
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Author: Harry Rosenbusch
Publisher: Forgotten Books
ISBN: 9781332059447
Category : Science
Languages : en
Pages : 354
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Book Description
Excerpt from Microscopical Physiography of the Rock-Making Minerals: An Aid to the Microscopical Study of Rocks In abridging the book, I have endeavored to retain all that appeared to be essential to a fair, general comprehension of the sub jcet. Omitting what seemed to be refinements beyond the need of the average student, and for which the advanced student is referred to the original work. Thus most of the historical portions have been omit ted, as well as the elaborate treatment of the optical anomalies of cer tain minerals, and many notes on European localities; while a number of notes on American occurrences have been inserted. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
