Seismo Lab Logo

Magnitude 5.8 offshore Cape Mendocino, CA

Information from the UCB & USGS Menlo Park
Location: 79 km from Punta Gorda
40.386 -125.279
Date & Time (Local): 2000/03/16
07:19:56
Date & Time (UTC): 2000/03/16
15:19:56
Depth (km): 7.8
Mw: (Preferred) 5.9
Ml: 5.8
Fault System: Mendocino Fault

This earthquake occurred in the most seismically active area in California. The Cape Mendocino region is part of a complex geological area, where the Pacific, North America, and Gorda plates meet, and is known as a "triple junction".

This area produces significant earthquakes on a regular basis. Long-time residents will remember the 1980 Trinidad earthquake (M7.1), which ruptured the Gorda plate in a left-lateral mechanism. This event injured 8 people and caused $1,750,000 in damage. The 1992 Cape Mendocino earthquake (M7.1) was a subduction zone earthquake, occuring at the boundary between the Gorda and North America plates. Because it occured on land, this event and its two large aftershocks caused 356 injuries and $48,300,000 in damage. In 1994, a M6.9 earthquake ocurred on the Mendocino fault zone, west of this event. Both the 1994 and the recent event show the right-lateral strike-slip mechanisms typically associated with this fault. More information on the 1994 earthquake can be found in this write-up from the USGS in Menlo Park. Several months later, a M6.6 earthquake occurred in the Gorda plate. Similar to the 1980 event, this earthquake showed a left-lateral strike-slip mechanism.


Return to the Events of Interest
Return to the Berkeley Seismological Laboratory

The Berkeley Seismological Laboratory, 202 McCone Hall, UC Berkeley, Berkeley CA 94720
Questions and comments to www@seismo.berkeley.edu
Copyright 2000, The Regents of the University of California.