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Magnitude 6.0 - CENTRAL CALIFORNIA
2004 September 28 17:15:24 UTC

Preliminary Earthquake Report
California Integrated Seismic Net
USGS/ Caltech/ CGS/ UCB/ UCSD/ UNR

This earthquake is the anticipated Parkfield earthquake, Mw 6.0 on the San Andreas fault. It ruptured roughly the same segment of the fault that broke in 1966. The earthquake occurred at 10:15 AM PDT on September 28, 2004. Its hypocenter was located at 35 degrees, 49 minutes north, 120 degrees 22 minutes west, at a depth of 8 km or 5 miles. From this point, about 7 miles SW of the town of Parkfield, it ruptured primarily northwest along the San Andreas fault. Strong shaking during this event lasted for about 10 seconds. This earthquake is the seventh in a series of repeating earthquakes on this stretch of the fault. The previous events were in 1857, 1881, 1901, 1922, 1934, and 1966.
Small Globe

Small map showing earthquake

Magnitude 6.0
Date-Time Tuesday, September 28, 2004 at 17:15:24 (UTC)
= Coordinated Universal Time
Tuesday, September 28, 2004 at 10:15:24 AM
= local time at epicenter

Location 35.815°N, 120.374°W
Depth 7.9 km (4.9 miles)
Region CENTRAL CALIFORNIA
Distances 11 km (7 miles) SSE (151°) from Parkfield, CA
18 km (11 miles) N (1°) from Shandon, CA
30 km (18 miles) ENE (76°) from San Miguel, CA
34 km (21 miles) NE (53°) from Paso Robles, CA
217 km (135 miles) SE (141°) from San Jose City Hall, CA
Location Uncertainty horizontal +/- 0.4 km (0.2 miles); depth +/- 0.6 km (0.4 miles)
Parameters Nst=248, Nph=248, Dmin=3 km, Rmss=0.11 sec, Gp= 94°,
M-type=regional moment magnitude (Mw), Version=7
Source California Integrated Seismic Net
USGS/ Caltech/ CGS/ UCB/ UCSD/ UNR
Event ID nc51147892

Organizations

For more information, go to http://quake.wr.usgs.gov/ || Contacts

The official magnitude for this earthquake is indicated at the top of this page. This was the best available estimate of the earthquake's size, at the time that this page was created. Other magnitudes associated with web pages linked from here are those determined at various times following the earthquake with different types of seismic data. Although, given the data used, they are legitimate estimates of magnitude, they are not considered the official magnitude.


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