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San Fernando, California, Earthquake of 9 February 1971
Excerpt from San Fernando, California, Earthquake of 9 February 1971
The southwestern, eastern, and extreme north eastern parts of the range contain meta sedimentary rocks that were extensively converted to gneiss and migmatite during intrusion Of Mesozoic granitic rocks. These rocks are in fault contact with rocks in the interior of the range.
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.
The southwestern, eastern, and extreme north eastern parts of the range contain meta sedimentary rocks that were extensively converted to gneiss and migmatite during intrusion Of Mesozoic granitic rocks. These rocks are in fault contact with rocks in the interior of the range.
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.
518 pages, Hardcover
Published February 13, 2018
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