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The 1983 Coalinga earthquake struck at 4:42 p.m. Monday, May 2 of that year, in Coalinga, California. The shock was felt from the Greater Los Angeles Area north to Susanville in Lassen County, and between the Pacific Coast and western Nevada. More than 5,000 aftershocks were recorded through July 31, of which 894 had a magnitude of 2.5 or larger.
At 2342 G.m.t. May 2, 1983, a magnitude (ML) 6.7 earthquake occurred about 12 km northeast of the town of Coalinga, approximately halfway between Los Angeles and San Francisco. The shock was felt from Los Angeles to 200 km north of Sacramento and as far east as Las Vegas.
Coalinga has had: (M1.5 or greater) 1 earthquake in the past 24 hours. 9 earthquakes in the past 7 days. 30 earthquakes in the past 30 days. 310 earthquakes in the past 365 days.
1983 Coalinga, California GEOS Data. This site contains earthquake and aftershock data collected by the United States Geological Survey (USGS) General Earthquake Observation System (GEOS) project in Menlo Park, California.
Effects of the 1983 Coalinga, California, earthquake on creep along the San Andreas fault. The M//L approximately equals 6. 5 earthquake that occurred near Coalinga, California, on May 2, 1983 induced changes in near-surface fault slip along the San Andreas fault.
16 Ιαν 2021 · The Coalinga earthquake was a 6.5 magnitude event on the Richter scale that struck downtown Coalinga on May 2, 1983 at 11:42 in the evening. The quake was caused when Anticline Ridge, just north and northeast of town, was pushed up and out to the south about 1 to 2 feet along a reverse fault, 10 km down, that forms the core of the fold, which ...
The 2 May 1983 Coalinga, California, earthquake (magnitude 6.5) failed to rupture through surface deposits and, instead, elastically folded the top few kilometers of the crust. The subsurface rate of fault slip and the earthquake repeat time are estimated from seismic, geodetic, and geologic data.
