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Geologic Section From The Sierra Nevada To Death Valley, California

Hopper, Richard H. (1947) Geologic Section From The Sierra Nevada To Death Valley, California. Geological Society of America Bulletin, 58 (5). pp. 393-432. ISSN 0016-7606. doi:10.1130/0016-7606(1947)58[393:gsftsn]2.0.co;2. https://resolver.caltech.edu/CaltechAUTHORS:20220204-246017300

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Abstract

This paper describes the geology of a part of the region between the southern Sierra Nevada and Death Valley, one of the most rugged portions of the Great Basin. The topographic features of the mountain ranges in this region strongly suggest that each range owes its present height to faulting. In the western half of the area mapped, displacements of extensive basalt flows of probable early Pleistocene age support the topographic evidences of faulting. On the summits of the ranges are areas of low relief, believed to be remnants of a single old-age erosion surface which extended across the entire region before the beginning of the range-forming fault movements. The undisturbed erosion which produced this surface ended shortly before the deposition of the fossiliferous late Pliocene or early Pleistocene Coso formation; therefore, this surface is tentatively correlated with the Ricardo erosion surface of the Mohave Desert region, which bevels tilted early Pliocene strata and which is also dislocated by range-forming faults. The ranges are composed dominantly of pre-Tertiary rocks. The pre-Cambrian metasediments, chiefly mica schists and dolomites, have an exposed thickness of 15,000 feet. Limestones, dolomites, shales, and quartzites of Paleozoic age are more than 30,000 feet thick, and fossils collected in them indicate the probable presence of all the Paleozoic systems. During the late Jurassic Nevadian orogeny the pre-Mesozoic rocks were folded, faulted, and intruded by plutonic bodies ranging from granite to gabbro. All the post-Mesozoic rocks are believed to be Miocene or younger; they include a wide variety of volcanic and sedimentary types. Most of the faulting to which the region owes its present relief occurred in the early or middle part of the Pleistocene, probably after the first (McGee) glacial stage in the Sierra Nevada. The activity on one of the major fault zones, however, has continued into the Recent epoch. All the range-forming faults whose attitudes could be determined are high-angle normal faults.


Item Type:Article
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URLURL TypeDescription
https://doi.org/10.1130/0016-7606(1947)58[393:gsftsn]2.0.co;2DOIArticle
Additional Information:© 1947 Geological Society of America. The writer acknowledges his indebtedness to Dr. L. F. Noble and Mr. R. P. Bryson, of the United States Geological Survey, and to Mr. H. D. Curry, of the United States National· Park Service, for suggestions regarding the geology of the Panamint Range. Thanks are also due Dr. Edwin Kirk, Mr. L. G. Henbest, and Dr. Josiah Bridge, of the United States Geological Survey, and especially to the late Dr. G. H. Girty, of the same organization, for identifications of the fossils collected. Finally, the writer expresses his gratitude to the staff of the Division of Geological Sciences of the California Institute of Technology, and particularly to Professor J.P. Buwalda, for valuable advice and criticism.
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological Sciences427
Issue or Number:5
DOI:10.1130/0016-7606(1947)58[393:gsftsn]2.0.co;2
Record Number:CaltechAUTHORS:20220204-246017300
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20220204-246017300
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:113269
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:04 Feb 2022 17:36
Last Modified:04 Feb 2022 17:36

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