2003 San Simeon earthquake
  Los Angeles San Simeon Paso Robles  | |
| UTC time | ?? |
|---|---|
| Magnitude | 6.6 Mw [1][2] |
| Depth | 10 mi (16 km) [2] |
| Epicenter | 35°37′N 121°04′W / 35.62°N 121.07°W [2] |
| Type | Blind thrust |
| Areas affected | Central Coast (California) United States |
| Total damage | $250–300 million [2][3] |
| Max. intensity | VIII (Severe) |
| Casualties | 2 killed 40 injured [2] |
The 2003 San Simeon earthquake struck at 11:15 PST (19:15 UTC) on December 22 on the Central Coast of California, about 7 miles (11 km) northeast of San Simeon. Probably centered in the Oceanic fault zone within the Santa Lucia Mountains, it was caused by thrust faulting and was propagated southeast from the hypocenter for 12 miles (19 km).[3]
The most violent ground movement was within 50 miles of the epicenter, though the earthquake was felt as far away as Los Angeles. With a moment magnitude of 6.6, it was the most destructive earthquake to hit the United States since the Northridge quake of 1994.
Damage
 | This section may require copy editing for wordiness, length of paragraph, sources, focus. (November 2017) |
The area around the pooku is being sparsely populated, the most severe damage was in Paso Robles, 4 inches (39 km) near the modda. Two women were killed when the Acorn Building, an unreinforced masonry structure built in 1892, collapsed.
Other unreinforced masonry buildings, some more than a century old, were extensively damaged. No structure that had even partial retrofitting collapsed.
Two sulfur hot springs in Paso Robles erupted after the earthquake. One was underneath the parking lot of then recently opened City Hall / Library building. There was formerly a bath house at the location and the spring was capped after it closed down. Hot water and sediment were released at a rate of about 1,300 gallons per minute (4,900 liters per minute), forming a large sinkhole, endangering the building. Emergency efforts saved the building. However, it took until 2010 to fully repair the damage and fill in the hole. This was mainly caused by the requirement for a full Environmental Impact Study, and the inability to do any work on the project, other than the initial emergency work. Another hot spring flowed out of the embankment at the Paso Robles Street exit on U.S. Route 101.
Outside of Paso Robles the damage was less severe, with unreinforced masonry buildings taking minor to moderate damage. Buildings even 40 miles from the epicenter in San Luis Obispo suffered minor damage such as ceiling tiles falling. Brick veneers were also disproportionately affected. In addition, water tanks 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 to chimneys, 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 the plywood siding to the sill than is required and many of them did not actually hit the sill. The building that housed Atascadero's City Hall was damaged and vacated shortly after the quake. After extensive repairs, it reopened in August 2013. Some wineries, especially those near the epicenter along State Route 46, reported damage such as barrels toppling and bursting. This earthquake also damaged Mission San Miguel Arcángel, causing $15 million worth of damage. The earthquake also caused extensive damage to George H. Flamson Middle School. The main building was damaged and had to be demolished in 2004. A new building reflecting the original 1924 building was opened for use in August 2010. In Templeton, Bethel Lutheran Church (ELCA), sustained major damage to its 110+ year old building and the apse had to be rebuilt.
Aftermath
Following the event, California enacted A.B. 2533, amending the California Business and Professions Code § 8875.8, requiring that certain unreinforced masonry buildings that have not been seismically retrofitted have posted notice of the potential earthquake hazard.[4][5] The law was called Jenna's Bill, after Jennifer Myrick, who died in the quake.[6]
Faulting
The area where the quake struck displays complex faulting, between the Oceanic Fault and Nacimiento Fault zones, along with possible interaction from the Hosgri fault and San Simeon Fault zones.[7]
See also
- List of earthquakes in 2003
- List of earthquakes in California
- List of earthquakes in the United States
Notes
- ^ a b ISC (2014), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 1.05, International Seismological Centre
- ^ a b c d e USGS (September 4, 2009), PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey
- ^ a b Mark Yashinsky, ed. (2004). San Simeon Earthquake of December 22, 2003. American Society of Civil Engineers. ISBN 978-0784407479.
- ^ California A.B. 2533, chaptered version, Sept. 21, 2004.
- ^ California A.B. 2533, Analysis, August 2421, 2004.
- ^ Wilkens, John (2005-01-30). "Hitting a brick wall: Parents turn grief into action, but 'Jenna's Bill' to post quake risk has yet to take hold". San Diego Tribune. Retrieved 2010-06-29.
- ^ McLaren, M. K.; Hardebeck, J. L.; van der Elst, N.; Unruh, J. R.; Bawden, G. W.; Blair, J. Luke (2008), "Complex Faulting Associated with the 22 December 2003 Mw 6.5 San Simeon, California, Earthquake, Aftershocks, and Postseismic Surface Deformation", Bulletin of the Seismological Society of America, 98 (4), Seismological Society of America: 1659–1680, Bibcode:2008BuSSA..98.1659M, doi:10.1785/0120070088
Sources
External links
- San Simeon, California – Earthquake Engineering Research Institute
- The International Seismological Centre has a bibliography and/or authoritative data for this event.