Installing a Tremorscope station. Click to view full-sized picture...
Until recently, active fault zones were thought to deform via seismic slip during earthquakes in the upper, brittle portion of the crust, and by steady, aseismic shear below. However, in the past decade, this view has been shaken by seismological observations of seismic tremor deep in the roots of active fault zones. First recognized on subduction zones in Japan and the Pacific Northwest, tremor has also been found to be very active on a short section of the San Andreas to the southeast of one of the most densely monitored fault segments in the world, near Parkfield (Nadeau and Dolenc, 2005). This deep (~20-30 km) zone of activity is located right below the nucleation zone of the great 1857 Fort Tejon earthquake. Thus, learning more about the temporally and spatially complex faulting processes in this zone may help us better understand the conditions that lead to such large ruptures.
The BSL's Tremorscope project is supported by grant from the Gordon and Betty Moore Foundation. Its goal is to improve our ability to observe and thereby learn more about the tremor which occurs in the region south of Parkfield, CA, and east of Paso Robles, CA. by installing eight additional high-fidelity seismic stations in the area.
With a grant from the Moore Foundation, the BSL is installing TremorScope, four borehole and four surface stations positioned to record deep tremor along the San Andreas Fault in central California. Above: recently discovered tremors (gold stars) and the location of the proposed stations, whose instrumentation will be used to study the behavior of faulting in the deep crust. Click to view full-sized map...
The last of the four planned surface stations was installed in June 2013, and data from them is already contributing to our tremor observations. The first step in the installation of the remaining four stations has just begun with the drilling of the first borehole. The deployment of the seismic equipment in boreholes at these sites will additionally reduce ambient noise.
Tremor Map and Catalog
TremorScope Seismo Blog posts
Project will monitor tremor activity beneath San Andreas Fault
December 9, 2010
UC Media Relations
by Robert Sanders
BERKELEY - The Berkeley Seismological Laboratory will begin early next year to install earthquake detectors on the southern San Andreas Fault near the town of Cholame to study mysterious tremors discovered beneath the area.
Tremors are extremely faint and periodic rumblings originating 20-40 kilometers below ground - far beneath the zone where earthquakes occur - that appear to be associated with slipping rocks deep in the earth.
UC Berkeley seismologists discovered the tremors in 2004 just south of the heavily instrumented Parkfield area of the fault, and subsequent studies suggest that changes in tremor activity may precede earthquakes. Tremors also have been detected in active earthquake zones in Japan and Washington state.
"The discovery of tremors deep in the roots of active plate boundary fault zones is arguably the most important discovery in earthquake science in decades," said Roland Bürgmann, principal investigator for the TremorScope project and professor and chair of UC Berkeley's Department of Earth and Planetary Science. "This is the first project in which a permanent instrument network has been specifically designed with tremor in mind."