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Geology Of The Pegmatites And Associated Rocks Of Maine

Geology Of The Pegmatites And Associated Rocks Of Maine

Edson Sunderland Bastin

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Editorial:
Kessinger Publishing
Año de edición:
2008
Materia
Biología celular (citología)
ISBN:
9781436857390
29,05 €
IVA incluido
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Geology Of The Pegmatites And Associated Rocks Of Maine: Including Feldspar, Quartz, Mica, And Gem Deposits (1911) is a comprehensive book written by Edson Sunderland Bastin. The book is focused on the geology of Maine, particularly the pegmatites and associated rocks found in the region. The author provides detailed information on the various types of rocks found in Maine, including feldspar, quartz, mica, and gem deposits. The book is divided into several chapters, each of which covers a different aspect of the geology of Maine. The first chapter provides an overview of the geology of the region, including its history and the various types of rocks found there. The subsequent chapters delve deeper into specific types of rocks, such as feldspar and quartz. The book also includes information on the various mining operations that have taken place in Maine throughout history. The author provides detailed accounts of the methods used to extract minerals from the ground, as well as the economic and social impact of these operations on the local communities. Overall, Geology Of The Pegmatites And Associated Rocks Of Maine: Including Feldspar, Quartz, Mica, And Gem Deposits (1911) is a valuable resource for anyone interested in the geology of Maine or the mining industry in general. The book is well-researched and provides a wealth of information on the various types of rocks found in the region.This scarce antiquarian book is a facsimile reprint of the old original and may contain some imperfections such as library marks and notations. 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 their original work.

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