1868 Hayward earthquake
The 1868 Hayward earthquake occurred in the San Francisco Bay Area, California, United States on October 21. With an estimated moment magnitude of 6.3–6.7 and a maximum Mercalli intensity of IX (Violent), it was the most recent large earthquake to occur on the Hayward Fault Zone. It caused significant damage and a number of deaths throughout the region, and was known as the "Great San Francisco earthquake" prior to the 1906 San Francisco earthquake and fire.
Santa Rosa Santa Cruz | |
UTC time | 1868-10-21 15:53 |
---|---|
USGS-ANSS | ComCat |
Local date | October 21, 1868 |
Local time | 07:53[1] |
Magnitude | 6.3–6.7 Mw[2] |
Epicenter | 37.7°N 122.1°W[3] |
Fault | Hayward Fault Zone |
Type | Strike-slip |
Areas affected | San Francisco Bay Area California United States |
Total damage | $350,000 / Moderate [4] |
Max. intensity | IX (Violent)[3] |
Casualties | 30[3] |
Earthquake
The earthquake occurred at 7:53 a.m. on October 21, 1868. Its epicenter was likely located near Hayward, California, and its magnitude has been estimated to have been 6.3–6.7 on the moment magnitude scale. At the surface, ground rupture was traced for 20 miles (32 km), from San Leandro to what is now the Warm Springs District in Fremont.[1]
Damage
The town of Hayward experienced the most damage, with nearly every building destroyed or significantly damaged in the earthquake. The Alameda County Courthouse in San Leandro was destroyed, which resulted in the re-location of the County Seat to Oakland, its current site. The adobe chapel of Mission San José in what is now Fremont was also destroyed, as were several buildings in San Jose, San Francisco and throughout Alameda County. Damage was reported from Santa Rosa in the north to Gilroy and Santa Cruz in the south. Thirty deaths were attributed to the earthquake.[1]
Intensity
The United States Geological Survey estimates that Hayward experienced shaking measuring IX (Violent) on the modified Mercalli scale. San Leandro experienced shaking measuring VIII (Severe), while San Francisco and Oakland experienced shaking measuring VII (Very strong).[5]
See also
References
- "Historic Earthquakes: Hayward, California, 1868 October 21 15:53 UTC". United States Geological Survey. 1993. Archived from the original on 5 November 2008. Retrieved 2008-10-15.
- Hough, S. E.; Martin, S. S. (2015), "The 1868 Hayward Fault, California, Earthquake: Implications for Earthquake Scaling Relations on Partially Creeping Faults", Bulletin of the Seismological Society of America, 105 (6): 2984, 2907, Bibcode:2015BuSSA.105.2894H, doi:10.1785/0120140372
- Stover, C.W.; Coffman, J.L. (1993). Seismicity of the United States, 1568–1989 (Revised). U.S. Geological Survey professional paper 1527. United States Government Printing Office. pp. 73, 104.
- National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Database (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K
- The 1868 Hayward Earthquake: 139 years and counting... (press conference). Hayward Area Historical and Society Museum: U.S. Geological Survey, Association of Bay Area Governments, Hayward Area Historical and Society Museum, Vice Mayor-City of Hayward. 17 October 2007. Retrieved 15 October 2008.
Further reading
- Aldrich, M. L.; Bolt, B. A.; Leviton, A. E.; Rodda, P. U. (1986), "The "Report" of the 1868 Haywards earthquake", Bulletin of the Seismological Society of America, 76 (1): 71–76, archived from the original on 2015-09-23, retrieved 2014-07-22
- Boatwright, J.; Bundock, H., Modified Mercalli Intensity Maps for the 1868 Hayward Earthquake Plotted in ShakeMap Format, Open-File Report 2008-1121, United States Geological Survey
External links
- 1868 Hayward Earthquake Alliance
- Images from the 1868 earthquake aftermath – The Bancroft Library
- Photos of damage in San Francisco following the 1868 earthquake – San Francisco Public Library
- Prepare for big ruptures on Hayward fault, scientists say – Stanford University
- The 150th Anniversary of the Damaging 1868 Hayward Earthquake: Why It Matters and How We Can Prepare for Its Repeat – Tom Brocher (USGS)