Geology Of The Central Portion Of The Rumsey Quadrangle California

Author : Russell B. Travis
Publisher : Forgotten Books
ISBN 13 : 9780656221608
Total Pages : 48 pages
Book Rating : 4.2/5 (216 download)

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Download or read book Geology of the Sebastopol Quadrangle, California (Classic Reprint) written by Russell B. Travis and published by Forgotten Books. This book was released on 2018-02-10 with total page 48 pages. Available in PDF, EPUB and Kindle. Book excerpt: Excerpt from Geology of the Sebastopol Quadrangle, California The rocks in the area, predominately sedimentary, range in age from Upper Jurassic to Recent. The oldest rocks, the franciscan-knoxville group, form the basement in the region and crop out primarily in the northwestern quarter of the quadrangle. They consist chiefly of sandstones of the graywacke type and interbedded shale, chert, and altered volcanic rocks; they have been intruded by diabase and serpentine. Meta morphic rocks of the glaucophane schist type are locally developed in the vicinity of serpentine and in a few places where no serpentine is apparent. In the southeastern part of the quadrangle, greenish clay of the Petaluma formation (middle or upper Pliocene) is in fault contact with franciscan-knoxville rocks. Both of the formations are unconformably overlain by the Merced formation (upper Pliocene) or by thin basalt flows which locally are interbedded with the Merced formation. The basalt flows are part of a thick series, the Sonoma volcanic rocks (upper Pliocene), which crop out primarily east of the Sebastopol quadrangle. The Merced formation, consisting chiefly of very fine-grained, massive, marine sandstone and some fresh water sand and gravel, forms a thin blanket over most of the central and southern part of the quadrangle. In many places it includes a thin bed of tuff-breccia. Overlying these formations are marine and river terrace deposits and valley alluvium. The franciscan-knoxville rocks are complexly folded and faulted, but some broad northwest - trending folds can be recognized. The Petaluma formation is Sharply folded, probably by the late Pliocene orogeny. The Merced formation has been broken by a series of high-angle faults as a result of Pleistocene uplift, northeast tilting, and settling movements of the San francisco-marin block which the quadrangle occupies. The large streams draining the area flow westward across the regional structure. Recent subsidence (or rise in sea level) is evidenced by the drowned mouths of these streams. 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.