February 22, 14:00 PST (updated 23 Feb):
A ML5.4 mainshock occurred at 04:19 am on 22 February,
located 2 miles north of Big Bear City in San Bernardino
County at a depth of 3.7 miles. It was not preceded by
foreshocks. It was followed by strong aftershock activity
of 116 aftershocks during the first 6 hours, with the five
largest aftershocks (local time):
- 22 Feb 04h 20 min M4.0
- 22 Feb 04h 21 min M4.3
- 22 Feb 04h 25 min M4.0
- 22 Feb 06h 16 min M4.1
- 22 Feb 11h 33 min M4.5
We use seismic records to determine the orientation of the
fault on which an earthquake occurs. The mainshock exhibited
strike-slip faulting (horizontal movement) on a steeply
dipping (80 degrees) plane striking N40W, sub-parallel
to the local strike of the Helendale fault. This mechanism
is consistent with the mainshock being near the Helendale
fault, a more than 40 mile long, late Quaternary fault in
the Mojave Desert. Preliminary locations of the aftershocks
appear to form a 2 miles long, northwest striking trend,
located 2 miles to the west of the main surface trace of
the Helendale fault. Hence, this sequence may be occurring
on a small sub-parallel fault, adjacent to the Helendale fault.
This sequence is located in a very seismically active area. It
is located about 6.2 miles due north of the epicenter of the
M6.2 Big Bear aftershock of Landers, which occurred on 28
June 1992. Two M5.3 and M5.4 Landers aftershocks occurred
about 3.1 miles to the northwest of the current activity
in November and December 1992. In February 2001 a M5.1
event occurred about 5 miles to the west of the current activity.
The 1992 Mw7.3 Landers and the 1999 Mw7.1 Hector Mine earthquakes
occurred in the Eastern California Shear Zone (ECSZ) that cuts
across the Mojave desert forming a 40 mile wide swath of crustal
deformation. The 1992 Landers earthquake was located towards the
middle of this zone, while 1999 Hector Mine earthquake occurred
near the eastern edge of the ECSZ. In contrast, the Helendale
fault forms the western edge of the ECSZ. It has contributed
to the generation of past temporal clusters of large earthquakes in the ECSZ.
Egill Hauksson, Kate Hutton, Lucy Jones, and Doug Given