User:Dawnseeker2000/Sandbox 5

The 1984 Morgan Hill earthquake (also known as the Halls Valley earthquake) occurred on April 24 at 13:15:21 local time in the Santa Clara Valley of Northern California in the United States. The strike-slip shock occurred on the Calaveras Fault and had a moment magnitude of 6.2 and a maximum Mercalli intensity of VIII (Severe). The epicenter was located near Mount Hamilton in the Diablo Range of the California Coast Ranges. Morgan Hill and other nearby communities sustained serious damage, with financial losses of at least US$7.5 million.

Tectonic setting

 * San Francisco Bay Area
 * Hayward
 * transform boundary
 * San Andreas Fault System

At more than 170 km in length, the Calaveras–Paicines Fault Zone is a section of the San Andreas Fault System in central California.

Earthquake
The earthquake occurred along the Calaveras Fault, with the epicenter 16 km northeast of San Jose. The shock was felt in Sacramento in California's central valley.

Rupture directivity.

.

Intensity
.

Strong motion
.

Ground effects
Landslide.

Ground failure and liquefaction.

Damage
Structural damage.

The earthquake was felt over an area of 120000 km2. Morgan Hill was strongly affected, with a number of mobile homes sliding off foundations, and moderate damage to several masonry buildings in the city. The communities of San Jose, San Martin and Coyote were some areas that experienced minor damage. In Santa Clara County, over 550 buildings were reported to have received at least minor damage.

Fires.

Residential
.

Commercial
.

Aftershocks
The outline of aftershocks show that the rupture propagated southeast over a 25 km section of the fault, as far as San Martin, to the location of the 1979 Coyote Lake earthquake's mainshock. That event's aftershock zone also stretched to the southeast.

Response
.

.