Description
Excerpt from The Minerals and Rocks of Arkansas: A Catalogue of the Species, With Localities and Notes
Igneous outcrops occur in Pulaski, Saline, Hot Springs, Montgomery, Pike and Sevier counties, and there is good reason for believing these igneous rocks are continuous beneath the drainage of the country. Another axis of disturbance shows a granitic out-crop on Spavinaw Creek in the Cherokee country, west of Benton county. The stratified rocks of Arkansas probably rest at no great depth upon an igneous platform.
In northern Arkansas the disturbance shows itself in small faults, gentle folds, and slightly indurated shales; but as you approach the granitic axis, greater faults, strata with high dip, and talcose slates intersected with quartz and calcite veins become common. These disturbances are intimately connected with, and determined the character of the mineral deposits of the State.
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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.
Igneous outcrops occur in Pulaski, Saline, Hot Springs, Montgomery, Pike and Sevier counties, and there is good reason for believing these igneous rocks are continuous beneath the drainage of the country. Another axis of disturbance shows a granitic out-crop on Spavinaw Creek in the Cherokee country, west of Benton county. The stratified rocks of Arkansas probably rest at no great depth upon an igneous platform.
In northern Arkansas the disturbance shows itself in small faults, gentle folds, and slightly indurated shales; but as you approach the granitic axis, greater faults, strata with high dip, and talcose slates intersected with quartz and calcite veins become common. These disturbances are intimately connected with, and determined the character of the mineral deposits of the State.
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.
Details
Publisher - Forgotten Books
Language - English
Hardback
Contributors
Author
F. L. Harvey
Published Date -
ISBN - 9780266251347
Dimensions - 22.9 x 15.2 x 0.2 cm
Page Count - 38
Paperback
Contributors
Author
F. L. Harvey
Published Date -
ISBN - 9781527788930
Dimensions - 22.9 x 15.2 x 0.2 cm
Page Count - 40
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