scholarly journals Supplemental Material: Prehistoric earthquakes on the Banning strand of the San Andreas fault, North Palm Springs, California

2021 ◽  
Author(s):  
B.A. Castillo ◽  
et al.

<div>Details of luminescence methods and results, and table of event indicators.<br></div>

2021 ◽  
Author(s):  
B.A. Castillo ◽  
et al.

<div>Plate 1. Plate provides photomosaics and mapping interpretations of excavations completed at 18th Avenue trench, including sample locations and interpreted event horizons. Annotations can be turned off through Layers function.<br></div>


2021 ◽  
Author(s):  
B.A. Castillo ◽  
et al.

<div>Plate 1. Plate provides photomosaics and mapping interpretations of excavations completed at 18th Avenue trench, including sample locations and interpreted event horizons. Annotations can be turned off through Layers function.<br></div>


2021 ◽  
Author(s):  
B.A. Castillo ◽  
et al.

<div>Details of luminescence methods and results, and table of event indicators.<br></div>


2020 ◽  
Author(s):  
Bryan Castillo ◽  
◽  
Sally McGill ◽  
Katherine M. Scharer ◽  
Doug Yule ◽  
...  

2019 ◽  
Author(s):  
Carol S. Prentice ◽  
◽  
Robert R. Sickler ◽  
Kevin B. Clahan ◽  
Alexandra Pickering ◽  
...  

1988 ◽  
Vol 78 (3) ◽  
pp. 1112-1122
Author(s):  
Patrick L. Williams ◽  
Sally Fagerson McGill ◽  
Kerry E. Sieh ◽  
Clarence R. Allen ◽  
John N. Louie

Abstract In addition to minor surface cracks in the region of the 8 July 1986 North Palm Springs earthquake, minor aseismic surficial rupture occurred along three segments of the San Andreas fault, 44 to 86 km southeast of the epicenter. Data from a creepmeter and a tiltmeter at one locality suggest that triggered slip occurred coseismically beneath the instruments but took 33 hr to propagate to the surface. That slippage occurred coseismically at depth favors mechanisms for triggered slip that involve dynamic or static strain changes rather than creep migrating from the source region. The distribution of slip along the San Andreas fault associated with the North Palm Springs earthquake differed significantly from that recorded after the moderate 1968 Borrego Mountain, California and 1979 Imperial Valley, California, earthquakes. During these earthquakes, triggered slip occurred along the San Andreas fault in the Durmid Hill area and in the Mecca Hills. Triggered slip associated with the North Palm Springs earthquake occurred in these two areas again, but also extended farther northwest into the Indio Hills, where as much as 9 mm of dextral slip occurred. In the Mecca Hills, surface cracks in 1986 appeared over a shorter fault length than in previous events, and the dextral displacement was smaller, with maximum values of only 2 to 3 mm. On Durmid Hill, surface cracks in 1986 were localized along a 200-m-long stretch of the fault spanning the Mecca Beach creepmeter and extending about 150 m to the southeast. Right-lateral displacements on surface cracks in this area were 1.4 to 2.0 mm, smaller than those observed in previous events. Although the mechanism of triggered aseismic slip is poorly understood, examination of displacement rates for the past several decades to centuries may indicate whether the aseismic slip rate is constant or represents accelerating premonitory failiure of the southernmost San Andreas fault.


Geosphere ◽  
2021 ◽  
Author(s):  
Bryan A. Castillo ◽  
Sally F. McGill ◽  
Katherine M. Scharer ◽  
Doug Yule ◽  
Devin McPhillips ◽  
...  

We studied a paleoseismic trench excavated in 2017 across the Banning strand of the San Andreas fault and herein provide the first detailed record of ground-breaking earthquakes on this important fault in Southern California. The trench exposed an ~40-m-wide fault zone cutting through alluvial sand, gravel, silt, and clay deposits. We evaluated the paleoseismic record using a new metric that combines event indicator quality and stratigraphic uncertainty. The most recent paleoearthquake occurred between 950 and 730 calibrated years B.P. (cal yr B.P.), potentially contemporaneous with the last rupture of the San Gorgonio Pass fault zone. We interpret five surface-rupturing earthquakes since 3.3–2.5 ka and eight earthquakes since 7.1–5.7 ka. It is possible that additional events have occurred but were not recognized, especially in the deeper (older) section of the stratigraphy, which was not fully exposed across the fault zone. We calculated an average recurrence interval of 380–640 yr based on four complete earthquake cycles between earthquakes 1 and 5. The average recurrence interval is thus slightly less than the elapsed time since the most recent event on the Banning strand. The average recurrence interval on the Banning strand is thus intermediate between longer intervals published for the San Gorgonio Pass fault zone (~1600 yr) and shorter intervals on both the Mission Creek strand of the San Andreas fault (~215 yr) and the Coachella section (~125 yr) of the San Andreas fault.


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