- 23 Jun 2021 13:06:07 PDT, (34.147, -116.445), depth 5.5km.
- 4km NNW of Yucca Valley, California
- As of 23 Jun 2021, 02:05PM PDT, there have been 2 aftershocks recorded.
- The largest was M1.9 (smallest M1.4).
- More 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.
- There were 2 events during the 3 days prior to the earthquake (within a 10 km radius).
- The largest was M1.1 (2021/06/23).
- Since our records began in 1932 we’ve had 97 events of M4 or greater within 10km of today’s event.
- The largest historic event was M7.3 on 1992/06/28.
- The most recent historic event was M4.0 on 06 Aug 2010.
- CFM fault associations: most likely Pinto Mountain fault (38%). Alternates: Other CFM faults (62%).*
- Nearby faults: Pinto Mountain fault zone (Pinto Mountain fault) (1.9 km), Johnson Valley fault, southern Johnson Valley section (Johnson Valley fault) (2.0 km), Pinto Mountan fault zone (3.8 km), Burnt Mountain fault zone (Burnt Mountain fault) (4.4 km), Eureka Peak fault (5.1 km), Pinto Mountain fault zone (Morongo Valley fault) (7.2 km), Johnson Valley fault, southern Johnson Valley section (9.3 km), Pipes Canyon fault (10.6 km) and Burnt Mountain fault zone (East Wide Canyon fault) (13.6 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.