Late Quaternary Faulting and Seismic Hazard in Southeastern Arizona and Adjacent Portions of New Mexico and Sonora, Mexico
Author
Pearthree, P.A.Issue Date
1986Keywords
Arizona Geological Survey Open File ReportsHolocene
late Pleistocene
mexico
Sonora
New Mexico
Arizona
fault movement
faulting
earthquake
seismic hazard
geomorphic
Geology
Quaternary
Pima County
Cochise County
Santa Rita
Safford
Basin and Range Province
Chiricahua fault
Peloncillo fault
Pitaycachi fault
Santa Rita Fault
climate change
fault scarp
recurrence rate
historic seismicity
Metadata
Show full item recordCitation
Pearthree, P.A., 1986, Late Quaternary Faulting and Seismic Hazard in Southeastern Arizona and Adjacent Portions of New Mexico and Sonora, Mexico. Arizona Geological Survey Open File Report, OFR-86-08, 22 p.Description
Geomorphic and Quaternary geologic studies provide data with which to assess seismic hazard in southeastern Arizona and adjacent New Mexico and Sonora, Mexico, where one large (M ~ 7 1/4) historic earthquake has occurred against a background of very low seismicity. Conclusions regarding the distribution and timing of late Quaternary faulting are based on (1) estimated ages of soils based on correlation with soils near Las Cruces in southern New Mexico; (2) use of surface age-fault offset relationships to constrain the age of most-recent fault movement and to estimate the frequency of movement along individual faults; and (3) morphologic analyses of fault scarps to estimate their ages. Individual late Quaternary faults in the region have surface rupture recurrence intervals on the order of 105 years. However, the major earthquake that occurred in 1887 in northeastern Sonora is evidently part of a series of 5 or 6 surface-rupturing earthquakes that have occurred since 20 ka in a N-S-trending zone straddling the Arizona-New Mexico border. Surface ruptures during the late Pleistocene (about 20-120 ka) occurred from near Tucson east to the border area, but the rate of surface rupture occurrence was evidently 4-25 times lower than during the past 20 kyo The rate of Holocenelatest Pleistocene surface-rupturing, while much lower than some portions of the northern Basin and Range province, evidently represents a burst of activity relative to the average long-term rate of faulting in southern Arizona.Additional Links
http://repository.azgs.az.gov/uri_gin/azgs/dlio/864Language
enSeries/Report no.
OFR-86-08Rights
Arizona Geological Survey. All rights reserved.Collection Information
Documents in the AZGS Document Repository collection are made available by the Arizona Geological Survey (AZGS) and the University Libraries at the University of Arizona. For more information about items in this collection, please contact azgs-info@email.arizona.edu.North Bounding Coordinate
32.7345South Bounding Coordinate
30.5083West Bounding Coordinate
-111.577East Bounding Coordinate
-108.721Collections
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