- 20 Jul 2020 15:01:53 PDT, (34.932, -119.038), depth 13.6km.
- 10km W of Grapevine, California
- As of 21 Jul 2020, 07:43AM PDT, there has been 1 aftershock recorded, M1.5.
- Aftershocks may be expected in the next few days, the largest expected is approximately 1 magnitude unit smaller than the mainshock.
- There is a small chance (about 5%) that a larger quake could occur, with the likelihood decreasing over time.
- Since our records began in 1932 we’ve had 98 events of M4 or greater within 10km of today’s event.
- The largest historic event was M7.5 on 1952/07/21.
- The most recent historic event was M4.2 on 22 Sep 2005.
- CFM fault associations: most likely Pleito fault (45%). Alternates: Not associated with a CFM modeled fault (42%), Other CFM faults (13%).*
- Nearby faults: Pleito fault zone, eastern Pleito section (Pleito fault) (4.5 km), Pleito fault zone, western Pleito section (Pleito fault) (6.5 km), unnamed faults (1952 earthquake fractures) (7.8 km), San Andreas fault zone, Cholame-Carrizo section (9.8 km), Wheeler Ridge fault zone (Wheeler Ridge fault) (9.9 km), Pleito fault zone, western Pleito section (Oak Hill thrust) (10.7 km), Big Pine fault zone, Lockwood Valley section (Lockwood Valley fault) (12.5 km), Big Pine fault zone, Lockwood Valley section (12.5 km), Frazier Mountain thrust system (North Frazier Mountain thrust) (12.9 km), Frazier Mountain Thrust System (Cuddy Canyon fault) (14.5 km) and Big Pine fault zone, Lockwood Valley section (South Lockwood Valley fault) (14.6 km).**
- Links for: USGS earthquake page, ShakeMap, DYFI, waveforms.
- Visit our special reports page for further information on local notable earthquakes.
Below are the waveform data associated with this event, as recorded in our Live Seismograms Feed.
*Earthquakes can occur both near or on major known faults, and in places where no clear fault zones are known. Using the statistical method of Evans et al. (in prep. 2019) the location and focal mechanism of this earthquake suggest the above association with modeled faults in the Community Fault Model (CFM) provided by the Southern California Earthquake Center (SCEC) and Harvard University. Note that the CFM fault association may be different from the nearby faults list. Differences may arise due to different fault databases, and because the CFM fault association uses the hypocenter with relation to subsurface 3-dimensional fault orientation models, while the nearby faults list utilizes mapped surface traces as they relate to the epicenter.
CFM Fault: SCEC CFM 5.0 Fault name and closest segment if available; The CFM is maintained by Harvard University, Dept of Earth & Planetary Sciences.
Probability: The probability in percent the earthquake is associated with this fault.
SCSN: Caltech/USGS Southern California Seismic Network
**U.S. Geological Survey and California Geological Survey, 2006, Quaternary fault and fold database for the United States, accessed 2015, from USGS web site: https://earthquake.usgs.gov/hazards/qfaults/
This information is subject to change as more up-to-date data become available.