Last updated June 26th, 2020
Event
- 24 Jun 2020 10:40:49 PDT, (36.447, -117.975), depth 4.7km.
- 18km SSE of Lone Pine, California
Aftershocks
- As of 25 Jun 2020, 07:31PM PDT, there have been 317 aftershocks recorded.
- The largest was M4.6 (smallest M0.7). We have recorded:
- 1 event M≥4
- 14 events M≥3
- 102 events M≥2
- 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.
Possible Foreshocks
- There were 87 events during the 3 days prior to the earthquake (within a 10 km radius).
- The largest was M4.6 (2020/06/23).
Historical Seismicity
- Since our records began in 1932 we’ve had 16 events of M4 or greater within 10km of today’s event.
- The largest historic event was M5.2 on 2009/10/03.
- The most recent historic event was M4.6 on 23 Jun 2020.
Faults
- CFM fault associations: most likely Independance; Sierra Nevada fault segment (64%). Alternates: Not associated with a CFM modeled fault (29%), Other CFM faults (7%).*
- Nearby faults: Owens Valley fault zone, 1872 rupture section (Owens Valley fault) (3.6 km), Owens Valley fault zone, 1872 rupture section (4.4 km), Southern Sierra Nevada fault zone, Haiwee Reservoir section (5.6 km), unnamed faults south side Owens Lake (12.3 km) and Southern Sierra Nevada fault zone, Independence section (Independence fault) (12.7 km).**
Additional Information
- 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 b
y 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.
