This webpage has been replaced by a new version and will be phased out in the future. Please use our new Real-time Earthquake Map to access the latest earthquake information and event details. The links to the World, US, and CA/NV maps that were in the navigation on the left side of the page have been replaced by the links at the top of the new Map. The Real-time Earthquake Map User Guide describes how to use the map and all its features.

2008 April 30 03:03:06 UTC

Earthquake Details

  • This event has been reviewed by a seismologist.
Location40.837°N, 123.499°W
Depth28.5 km (17.7 miles)
Distances50 km (30 miles) WNW of Weaverville, California
55 km (35 miles) E of Eureka, California
60 km (40 miles) ENE of Fortuna, California
305 km (190 miles) NW of SACRAMENTO, California
Location Uncertaintyhorizontal +/- 0.4 km (0.2 miles); depth +/- 1.4 km (0.9 miles)
ParametersNST=140, Nph=140, Dmin=20 km, Rmss=0.15 sec, Gp= 54°,
M-type=regional moment magnitude (Mw), Version=7
Event IDnc40216664
  • Did you feel it? Report shaking and damage at your location. You can also view a map displaying accumulated data from your report and others.

Earthquake Summary

Small globe showing earthquakeSmall map showing earthquake

Felt Reports

Felt (VI) at Big Bar; (V) at Burnt Ranch, Hoopa, Junction City and Willow Creek; (IV) at Blue Lake, Douglas City, Forks of Salmon, Hayfork, Hyampom, Lewiston, Orleans, Redway, Salyer, Somes Bar, Weaverville and Yreka. Felt as far north as Crescent City, as far east as Fall River Mills and as far south as Leggett.

Tectonic Summary

The magnitude (M) 5.4 earthquake that occurred on Wednesday, April 30, 2008 at 03:03:06 UTC (Tuesday, April 29, 2008 at 08:03:06 PM PDT) located at a depth of 28.5 km (17.7 miles). Both the moment tensor and first-motion fault plane solution indicate that the earthquake had a "normal" mechanism. By comparison of this quake's depth with the depth of background seismicity recorded since 1974 (map and cross-section), it is apparent that the quake occurs below the Gorda - North America plate interface.

Earthquakes that occur on the plate interface would likely have a "reverse" mechanism, such as observed in the April 25, 1992 M7.2 Cape Mendocino earthquake near Petrolia. The depth and mechanism of the April 30 quake indicate that it occurred within the Gorda plate and not on the plate boundary. The mechanism of the April 30 quake is also similar to those of previous, smaller quakes east of the Mendocino Triple Junction which also show normal mechanisms. Normal mechanisms likely reflect bending stresses within the subducting Gorda plate.

Historically, the closest M>5 earthquake to the April 30 earthquake occurred on 1954/12/21 19:56:29.00 UTC with a M=6.5. The quake locates 32 km to the WSW of the April 30 earthquake. Seismic instrumentation in 1954 was quite sparse, and therefore its depth is poorly determined. However, relocations of the quake indicate that it likely occurred at shallower depth that the April 30 quake.

Earthquake Information for California

Additional Information