- 2003 San Simeon earthquake
earthquake
title=2003 San Simeon earthquake
date=December 22 ,2003
magnitude=6.6 Mw
depth= convert|7.6|km|mi|0
countries affected=Flag|United States (California )
location = coord|35.706|N|121.102|W
intensity = VIII - Destructive
casualties=2 killed
40 injuredThe 2003 San Simeon Earthquake was a magnitude 6.6
earthquake on theCentral Coast of California , about 7 miles northeast of San Simeon. It occurred at 11:15 PST (19:15UTC ) onDecember 22 ,2003 . The earthquake probably occurred on the Oceanic fault zone in theSanta Lucia Mountains . It was caused byreverse fault ing and propagated southeast from thehypocenter for 12 miles (19 km).The area around the
epicenter is sparsely populated and the most severe damage occurred in Paso Robles, 24 miles (39 km) east-northeast, where the earthquake's only fatalities occurred. The Acorn Building, anunreinforced masonry building built in 1892, completely collapsed, killing two women, one Jennifer Myrick, and one Marilyn Frost-Zafuto. Other unreinforced masonry buildings, some more than a century old, in the city's historic downtown area also had extensive damage. However, none of the buildings that had even partial retrofitting collapsed. There was a wrongful death lawsuit filed by the relatives of the deceased women against Mary Mastagni, and several trusts which owned the Acorn Building. The jury found Mastagni negligent in the care and maintenance of the Acorn Building and awarded nearly 2 million dollars to the plaintiffs.Two sulfur
hot spring s in Paso Robles erupted after the earthquake. One was underneath the parking lot of City Hall. Hot water andsediment were released at a rate of about 1,300 gallons per minute (4,900 liters per minute), forming a largesinkhole . There was formerly abath house at the location and the spring was capped after it closed down. Another hot spring flowed out of the embankment at the Paso Robles Road exit on U.S. Route 101.Outside of Paso Robles the damage was less severe, with unreinforced masonry buildings taking minor to moderate damage.
Brick veneers were also disproportionately affected. In addition,water tank s in Paso Robles, Templeton and Los Osos were damaged. Residential buildings, predominantly one to two story wood frame structures, weathered the quake with little or no damage. The damage that did occur was mostly limited tochimney s, although a house in Atascadero suffered severe damage when it moved off its foundation. The damage was probably caused by poor construction. There were fewer nails connecting theplywood siding to the sill than is required and many of them did not actually hit the sill. Some wineries, especially those near the epicenter along State Route 46, reported damage such as barrels toppling and bursting.References
* [http://www.cisn.org/special/evt.03.12.22/prelimreport.html California Integrated Seismic Network]
* [http://www.eeri.org/lfe/pdf/usa_san_simeon_eeri_preliminary_report.pdf Earthquake Engineering Research Institute] (PDF)
* [http://neic.usgs.gov/neis/poster/2003/20031222.html United States Geological Survey]External links
* [http://www.eeri.org/lfe/usa_san_simeon.html 6.5 San Simeon Earthquake Photo Galleries and Links]
* [http://ceenve.calpoly.edu/goel/san_simeon_eqk/index.html Cal Poly]
* [http://peer.berkeley.edu/san_simeonEQ/index.html University of California, Berkeley]
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