Intermediate (Quartz Monzonitic) Character of the Central and Southern Appalachian Granites: With a Comparative Study of the Granites of New England and the Western United States (Classic Reprint)
Intermediate (Quartz Monzonitic) Character of the Central and Southern Appalachian Granites: With a Comparative Study of the Granites of New England and the Western United States (Classic Reprint)
Excerpt from Intermediate (Quartz Monzonitic) Character of the Central and Southern Appalachian Granites: With a Comparative Study of the Granites of New England and the Western United States Feldspar, quartz, and biotite, in the order named, are the dominant minerals in these rocks throughout the region. The total feldspar varies greatly in amount, but ranges between per cent. (maryland) and per cent. (georgia), with an average for the entire region Of per cent. Of the total rock mass. Averaged for the individual states, ...
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Excerpt from Intermediate (Quartz Monzonitic) Character of the Central and Southern Appalachian Granites: With a Comparative Study of the Granites of New England and the Western United States Feldspar, quartz, and biotite, in the order named, are the dominant minerals in these rocks throughout the region. The total feldspar varies greatly in amount, but ranges between per cent. (maryland) and per cent. (georgia), with an average for the entire region Of per cent. Of the total rock mass. Averaged for the individual states, a nearly progressive increase in feldspar from north to south (maryland, 5453 per cent.; Virginia, per cent; North Carolina, per cent; South Carolina, 6684 per cent; and Georgia, per cent.) is indicated, the northernmost state, Maryland, showing the minimum, and the southernmost state, Georgia, the maximum amount. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at ... 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.
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