PENNSYLVANIA GLACIATION 1ST PH


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Pennsylvania Glaciation, First Phase


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Pennsylvania Glaciation First Phase


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Excerpt from Pennsylvania Glaciation First Phase: Materials for a Discussion of the Attenuated Border of the Moraine Described in Volume Z of the Second, Geological Survey of Pennsylvania Native copper and crystalline rocks are found only in the extreme eastern and western parts of Pennsylvania in the drift of this Phase. In both localities floating ice seems to have played an important part. With no intention of claiming a Lake Superior origin for the Connecticut and Eastern Pennsylvania copper, the latter can not come from the Trias entirely, as it is found in Monroe County, north of Kittatinny Mountain. Western Pennsylvania copper certainly has a Keewatin origin, and the specimen was berg-carried. 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.




Pennsylvania Glaciation, First Phase; Materials for a Discussion of the Attenuated Border of the Moraine Described in Volume Z of the Second Geologic


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Pennsylvania and the Ice Age


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The Glacial Geology of a Part of Northwestern Pennsylvania


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This investigation was conducted as the first part of a program to study the glacial geology of northwestern Pennsylvania ... Field work and laboratory investigations have been conducted with the aim to determine the stratigraphic relationships and the specific character of the various tills in the area. Mapping of kames, valley trains and such features was included to give a complete picture of the surficial geology. For this reason most attention is given to the character, distribution, and age relations of the tills.




Pennsylvania and the Ice Age


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