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Desert Hot Springs earthquake 1984

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Journal Article
Published: 01 August 2009
Bulletin of the Seismological Society of America (2009) 99 (4): 2190–2207.
... concealed beneath Quaternary alluvium, except locally where it disrupts Holocene alluvium along discontinuous scarps ( Clark, 1984 ). Southeast of Desert Hot Springs, along Miracle Hill, the Mission Creek fault forms more continuous scarps in Quaternary sediments (Fig.  3 ), and northwest of Desert Hot...
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Journal Article
Published: 01 December 1986
Bulletin of the Seismological Society of America (1986) 76 (6): 1838–1843.
.... Cox B. F. (1985) . Distribution and geologic relations of fault systems in the vicinity of the Central Transverse Ranges, southern California , U.S. Geol. Surv., Open-File Rept. 85-365 , 23 pp. Proctor R. J. (1968) . Geology of the Desert Hot Springs-upper Coachella Valley...
Journal Article
Published: 01 December 1993
Bulletin of the Seismological Society of America (1993) 83 (6): 1721–1743.
... of the Desert Hot Springs—Upper Coachella Valley area, California , Special Report 94 , Calif. Div. Mines and Geol. Scherbaum F. (1987) . Seismic imaging of site response using microearthquake recordings. Part II. Application to the Swabian Jura, southwest Germany, seismic network , Bull...
Journal Article
Published: 01 October 1996
Bulletin of the Seismological Society of America (1996) 86 (5): 1331–1349.
...-Anderson recordings indicate a local magnitude of M L 6.0. The 1948 Desert Hot Springs earthquake produced waveforms similar to 1986, although amplitudes for 1948 are typically 20 to 30% larger. The 1948 mainshock is relocated at 33°N55.2′, 116°W28.9′, with a focal depth of 12 km, a revised magnitude of M...
Journal Article
Published: 01 October 2002
Bulletin of the Seismological Society of America (2002) 92 (7): 2841–2860.
... to Desert Hot Springs. ( Keller et al. , 1982 ; Clark, 1984 ). Northwest of Desert Hot Springs, convincing evidence of Holocene activity is sparse ( Clark, 1984 ), and within the San Bernardino Mountains, the fault is overlain by unfaulted Quaternary deposits ( Matti et al. , 1985 ). Conversely...
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Journal Article
Journal: Geosphere
Published: 06 May 2021
Geosphere (2021)
... between them are consistent with a pull-apart basin, which and the 1948 Mw 6.3 Desert Hot Springs earthquake. Aftershocks of the 1986 likely formed as a result of a small right step in the Banning strand that is evi- event define a nearly planar surface that strikes N60 70°W, is ~15 km in length, dent...
Journal Article
Published: 15 July 2014
Bulletin of the Seismological Society of America (2014) 104 (4): 1989–2006.
... by seismic imaging, Delmarva Peninsula, Virginia, USA , J. Geophys. Res. 113 , no.  B08413 , doi: 10.1029/2007JB005421 . Catchings R. D. Rymer M. J. Goldman M. R. Gandhok G. ( 2009 ). San Andreas fault geometry at Desert Hot Springs, California and its effects on earthquake...
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Journal Article
Journal: Geosphere
Published: 19 December 2019
Geosphere (2020) 16 (1): 435–455.
... and Niemi, 2017 ). The youngest volcanic unit in the Sevier Desert is the Ice Springs basalt ( Fig. 3 ). The Ice Springs basalt is commonly reported as being 660 ± 170 14 C yr B.P. or younger ( Valastro et al. 1972 ; Oviatt, 1991 ; McBride et al., 2015 ). This age, however, is not considered robust...
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Journal Article
Published: 16 June 2015
Bulletin of the Seismological Society of America (2015) 105 (4): 2070–2080.
... of the fault in 1966 and 2004; a number of earlier earthquakes in the M  5.5–6.5 range may have also occurred there, many of them in the latter half of the nineteenth century ( Toppozada et al. , 2002 ). Finally, the San Gorgonio Pass area of the SSAF system ruptured in the 1948 M  6.0 Desert Hot Springs...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2005
GSA Bulletin (2005) 117 (3-4): 334–353.
... somewhat smaller, shorter lived, and more disrupted by younger Basin and Range normal faults, is similar to the buried Sevier Desert detachment system beneath central Utah. Both top-to-the-west systems formed near the transition between the Sevier thrust belt and its hinterland, collapsed broad thrust...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2001
GSA Bulletin (2001) 113 (7): 895–907.
... is equivalent to a minimum throw of 7.8 km for a 60° dip, and 4.5 km for a 30° dip. Nielson et al. (1986) estimated that slip on the Cave Canyon detachment began at 7 km depth, from a comparison of the estimated present-day geothermal gradient at Roosevelt Hot Springs in the northern Mineral Mountains...
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Journal Article
Journal: GSA Bulletin
Published: 01 August 2000
GSA Bulletin (2000) 112 (8): 1264–1279.
... of the Mendocino triple junction as it passed northward through Mojave Desert latitudes (e.g., Ingersoll, 1982 ; Glazner and Bartley, 1984 ) and thus may not require thickening to undergo extension. More problematic for extension-driven volcanism is the probable lack of extensively volatile-enriched mantle...
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Journal Article
Published: 01 May 2007
Environmental and Engineering Geoscience (2007) 13 (2): 99–160.
... were destroyed. Brush fires are difficult to control, especially if “Santa Ana” wind conditions are present. Santa Ana winds are hot, dry winds that blow from the inland desert toward the coast. When sustained winter rains saturate the denuded hillsides after a brush fire, landslides and debris flows...
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Journal Article
Published: 01 December 1988
Bulletin of the Seismological Society of America (1988) 78 (6): 1907–1929.
.... (1986) . Aftershocks of the 1986 North Palm Springs earthquake and relocation of the 1948 Desert Hot Springs earthquake sequence (abstract) , EOS 67 , 1089 . Prodhel C. (1979) . Crustal structure of the Western United States , U.S. Geol. Surv. Profess. Paper 1034 , 74 pp...
Journal Article
Published: 01 October 2002
Bulletin of the Seismological Society of America (2002) 92 (7): 2555–2601.
... newspaper and other reports, indicate M 5.8. This magnitude contrasts with the unreasonably high M 6.4–6.9 suggested by Rogers and Halliday ( 1992 ), who assumed that 10–13 km of poorly documented fissures indicated Calaveras fault rupture. The 1984 Morgan Hill earthquake of M 6.2, which had stronger...
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Journal Article
Journal: Palynology
Published: 01 July 2016
Palynology (2016) 40 (2): 145–159.
... ended and before the collapse). Since the palynological assemblages included spring-blooming plants (such as Olea europaea and Sarcopoterium spinosum ) and no common regional autumn bloomers (e.g. Artemisia ), it is proposed that the kiln went out of use due to the early June 659 CE earthquake. We also...
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Journal Article
Published: 21 July 2020
Bulletin of the Seismological Society of America (2020) 110 (4): 1427–1456.
... and an alignment of hot springs along its traces. Individual structures within the fault zone strike north–south in left‐stepping en echelon patterns and express both normal and right‐slip offsets, with grabens that are ∼ 2    km wide between adjacent faults ( Roquemore, 1981 ). A few kilometers east...
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Journal Article
Journal: GSA Bulletin
Published: 01 May 2010
GSA Bulletin (2010) 122 (5-6): 843–854.
... by relatively hot-humid summers and cold-dry winters. The East Asian winter monsoon, primarily controlled by the Siberian High, drives strong northwestern winds below 2000 m altitude from December to April in this area. This monsoon system is overlain by the westerlies above an elevation of 2–3 km ( Chang, 1972...
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Journal Article
Published: 01 July 2000
Seismological Research Letters (2000) 71 (4): 401–422.
... are listed in Table 7 . TABLE 7 Joshua Tree/Landers/Big Bear Aftershocks Location Magnitude Date Big Bear City 3.4 1/24 ” 4.2 ( Figure 3 , #13) 9/20 ” 2.5 9/27 Desert Hot Springs 3.5 3/4 ” 3.1 4/24 ” 3.2 9/11 Yucca Valley 3.1 4/2 ” 3.1 6/14...
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Journal Article
Published: 10 March 2015
Bulletin of the Seismological Society of America (2015) 105 (2A): 511–543.
... as such), and Data Type indicates whether it is a historical event (Hist) or from paleoseismology (Paleo). This dataset is also available with references from sources in Data and Resources . * The value of 1984 for UCERF3 represents the 1984 Morgan Hill earthquake, which only ruptured ∼40% of the parent fault...
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