Bulletin of the Seismological Society of America
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Bulletin of the Seismological Society of America; October 1934; v. 24; no. 4; p. 345-384
© 1934 Seismological Society of America
This Article
Right arrow Full Text (PDF)
Right arrow References
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by GIANELLA, V. P.
Right arrow Articles by CALLAGHAN, E.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

The Cedar Mountain, Nevada, earthquake of December 20, 1932*

VINCENT P. GIANELLA and EUGENE CALLAGHAN

UNIVERSITY OF NEVADA UNITED STATES GEOLOGICAL SURVEY

Abstract

The Cedar Mountain, Nevada, earthquake took place at about 10h 10m 04s p.m., December 20, 1932. It was preceded by a foreshock noted locally and followed by thousands of aftershocks, which were reported as still continuing in January 1934. No lives were lost and there was very little damage.

The earthquake originated in southwest central Nevada, east of Mina. A belt of rifts or faults in echelon lies in the valley between Gabbs Valley Range and Pilot Mountains on the west and Cedar Mountain and Paradise Range on the east. The length of this belt is thirty-eight miles in a northwesterly direction, and the width ranges from four to nine miles. The rifts consist of zones of fissures which commonly reveal vertical displacement and in a number of places show horizontal displacement. The length of the rifts ranges from a few hundred feet to nearly four miles, and the width may be as much as 400 feet. The actual as well as indicated horizontal displacement is represented by a relative southward movement of the east side of each rift. The echelon pattern of the rifts within the rift area indicates that the relative movement of the adjoining mountain masses is the same. The direction of relative horizontal movement corresponds to that along the east front of the Sierra Nevada at Owens Valley and on the San Andreas rift.

Footnotes

* [Published by permission of the Director, United States Geological Survey. Received for publication January 27, 1934.]




This article has been cited by other articles:


Home page
Bulletin of the Seismological Society of AmericaHome page
Historic Surface Faulting and Paleoseismicity in the Area of the 1954 Rainbow Mountain-Stillwater Earthquake Sequence, Central Nevada
Bulletin of the Seismological Society of America, August 1, 2004; 94(4): 1255 - 1275.



Home page
Bulletin of the Seismological Society of AmericaHome page
S. J. Caskey, S. G. Wesnousky, P. Zhang, and D. B. Slemmons
Surface faulting of the 1954 Fairview Peak (MS 7.2) and Dixie Valley (MS 6.8) earthquakes, central Nevada
Bulletin of the Seismological Society of America, June 1, 1996; 86(3): 761 - 787.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
T. OHMACHI and S. MIDORIKAWA
Ground-motion intensity inferred from upthrow of boulders during the 1984 Western Nagano Prefecture, Japan, earthquake
Bulletin of the Seismological Society of America, February 1, 1992; 82(1): 44 - 60.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
D. I. DOSER
Foreshocks and aftershocks of large (M greater double equals 5.5) earthquakes within the western Cordillera of the United States
Bulletin of the Seismological Society of America, February 1, 1990; 80(1): 110 - 128.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
D. I. DOSER and R. B. SMITH
An assessment of source parameters of earthquakes in the cordillera of the western United States
Bulletin of the Seismological Society of America, October 1, 1989; 79(5): 1383 - 1409.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
B. A. BOLT and R. A. HANSEN
The upthrow of objects in earthquakes
Bulletin of the Seismological Society of America, October 1, 1977; 67(5): 1415 - 1427.
[Abstract] [PDF]


Home page
Quarterly Journal of the Geological SocietyHome page
J. GILLULY
The tectonic evolution of the western United States: SEVENTEENTH WILLIAM SMITH LECTURE
Quarterly Journal of the Geological Society, February 1, 1963; 119(1-4): 133 - 174.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
D. TOCHER
Earthquake energy and ground breakage
Bulletin of the Seismological Society of America, April 1, 1958; 48(2): 147 - 153.
[Abstract] [PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
D. TOCHER
The Dixie Valley-Fairview Peak earthquakes of December 16, 1954: Introduction
Bulletin of the Seismological Society of America, October 1, 1957; 47(4): 299 - 300.
[PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
B. GUTENBERG
Mechanism of faulting in southern California indicated by seismograms
Bulletin of the Seismological Society of America, October 1, 1941; 31(4): 263 - 302.
[PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
E. CALLAGHAN and V. P. GIANELLA
The earthquake of January 30, 1934, at Excelsior Mountains, Nevada
Bulletin of the Seismological Society of America, April 1, 1935; 25(2): 161 - 168.
[PDF]


Home page
Bulletin of the Seismological Society of AmericaHome page
P. BYERLY
The first preliminary waves of the Nevada earthquake of December 20, 1932
Bulletin of the Seismological Society of America, January 1, 1935; 25(1): 62 - 80.
[Abstract] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 1934 by the Seismological Society of America.