Geology and Ore Deposits of Ainsworth Mining Camp, British Columbia (Classic Reprint)


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Excerpt from Geology and Ore Deposits of Ainsworth Mining Camp, British Columbia The principal producing mines in the district are the Bluebell on the east shore of the lake, No. 1, Florence, and the Highland; but several other minor properties ship irregularly. The field Work in connexion with this report was not confined to the actual mining camp of Ainsworth, but, in order to-solve the problems which demanded attention, the region to the north and south was examined with the result that the formations in Ainsworth and around Kaslo have been correlated. A study was made of the geology of the walls of the trench from Kaslo as far south as the International Boundary, and new information has been collected which bears on the origin of the Purcell trench, as the valley containing Kootenay lake is called. 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.




Ore Deposit Models


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Geology and Ore-Deposits of Rossland, B. C


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Excerpt from Geology and Ore-Deposits of Rossland, B. C: Submitted in Partial Fulfilment of the Requirements of the Degree of Doctor of Philosophy in the Faculty of Pure Science, Columbia University The relationship between diorite porphyry and monzonite is a doubtful one. The two are often found in contact in the mine-workings. But so intimately associated and so like in appear ance that the relative age is uncertain. The diorite porphyry is very frequently found lying between augite porphyrite and monzonite. But so far no intrusions of diorite porphyry into monzonite have been found underground. A dyke-like mass of it on the surface near the drill hall is possibly a roof pendant unabsorbed in the monzonite batholith. Both mica and non-mica dykes cut the diorite porphyry. And it is also intruded by dyke representatives of the later granitic intrusives. 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.




Geology and Ore-deposits of Rossland, B.C. [microform]


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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. To ensure a quality reading experience, this work has been proofread and republished using a format that seamlessly blends the original graphical elements with text in an easy-to-read typeface. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.




Gypsum in Canada


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Mesozoic Assembly of the North American Cordillera


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"In this well-illustrated book, Hildebrand expands upon his model for the development of the North American Cordillera detailed in Special paper 457. Starting with an overview of Cordilleran geology he goes on to provide an in depth look at how the Rubian ribbon continent was assembled. He integrates the complex geology of the Cordillera into an actualistic model involving arc magmatism, arc-continent collision, slab failure magmatism, and transcurrent motion in both Rubia and the western North American margin. While much of the focus is on the assembly of the Rubian ribbon continent, Hildebrand explores its interactions with North America during the Sevier and Laramide events and concludes that North America was the lower plate in both"--Provided by publisher.




Cordillera and Pacific Margin


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This document contains many reports comparable in scope and subject matter to those appearing in scientific journals and other serials. Most contributions include an abstract and a bibliographic citation. Subjects include stratigraphy, geology and sedimentology for the Cordillera and Pacific Margin.




Down the Columbia


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Originally published in 1921, Freeman's account of his journey down the Columbia river depicts in detail the natural beauty of the area and provides a glimpse at life along the river during the 1920's. The narrative traces his voyage from the headwaters of the Columbia to the run past Palisade Rock




Skarns in British Columbia


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Skarns in British Columbia have historically been important sources of iron, tungsten, copper, and gold. This publication begins with an introduction on skarn terminology and the problems of skarn identification. It then reviews a genetic model of skarn formation and presents descriptive profiles of eight types of skarn deposits; describes the database of at least 735 skarn occurrences in the province, and the number and distribution of skarns in British Columbia according to their associations, class, age, and distribution; and notes the ages of British Columbia skarns and the total production of various metals extracted from British Columbia skarns. Subsequent sections provide information on assays and metal ratios of mineralized skarns, skarn mineralogy, skarn mineral chemistry, chemistry of skarn-related intrusions, and the mapping and evaluation of skarns. The appendix contains a listing of 735 skarn occurrences in British Columbia, giving deposit name, MINFILE number, latitude/longitude, elements and minerals present, and associated rocks and their ages.




Tectonics, Metallogeny, and Discovery


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This summary report commences with a brief metallogenic overview of the northern Pacific Rim, with particular attention paid to the world-class Mesozoic and Cenozoic ore deposits that define the region's premier metallogenic provinces. This is followed by a summary of the relative attractiveness of the region's various mining jurisdictions, as recorded by recent exploration activity.