The Journal of Geology; Volume 13


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The Journal of Geology is a respected peer-reviewed scientific publication that has been in continuous publication since 1893. The journal publishes original research articles and reviews on a wide range of geological topics, including petrology, geochemistry, and paleontology. This journal is an essential resource for geologists, earth scientists, and researchers in related fields. 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 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. 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.




The Journal of Geology;


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.




The Journal of Geology, Vol. 29


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Excerpt from The Journal of Geology, Vol. 29: A Semi-Quarterly Magazine of Geology and Related Sciences; January-December, 1921 Geariticline do not move at the same rate, and the upper parts which were originally above the downward-moving secondary geosyncline may in a later stage Of evolution be above the. 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.




The Journal of Geology, 1905, Vol. 13 (Classic Reprint)


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Excerpt from The Journal of Geology, 1905, Vol. 13 Reviews: Vermont Geological Survey: Mineral Industries and Geology of Certain Areas, George H. Perkins (a. R. 375; The Manu facture of Hydraulic Cements, Albert Victor Bleininger (g. C 376; Preliminary Report on the Ohio Co-operative Topographic Survey, C. E. Sherman (g. C. 377. 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.




Collected papers


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Bulletin


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The American Geologist, Vol. 13


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Excerpt from The American Geologist, Vol. 13: A Monthly Journal of Geology and Allied Sciences; January to June, 1894 But while Dr. Lapham was a scientist, in the broad sense of the word, he was specially a geologist, and it is because of his alliance with science through the avenues of geological work that we desire to review succinctly his life and work in this series of sketches. 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.




The Journal of Geology, 1905


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Excerpt from The Journal of Geology, 1905, Vol. 13 The study of river action has been very much advanced in the Alps, whose torrents give magnificent examples of the destructive and constructive action of running water. But the surface features of this great European mountain chain do not all correspond to those which we might expect after a careful study of river action. Rivers seek to establish a normal curve, which grows continually gentler down-stream. The valleys of the Alps, however, do not show such a regular grade. The floors of the headwaters show many irregularities, and gentle grades alternate with steep ones. Instead of a slope curve, there is a succession of descending steps. Farther down we find for several miles a valley floor sloping normally; this floor has been aggraded by the river and often ends in a lake basin, where the normal slope is changed into a reversed one. Most of these features are not produced, but rather are destroyed, by river action. Indeed, we see how the rivers intrench themselves in the steep parts of the stair slope, and how they fill up the lakes, which generally occupy the lower part of their valleys in the Alps. In short, their action is directed toward removing the irregularities of their courses. There is still one other important point in which the slope of Alpine valleys does not obey those rules which control normal valleys; the law of Playfair is not applicable to them. 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.