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2017 Napa earthquake

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2017 Napa earthquake
Name2017 Napa earthquake
Date2017-08-24
Time10:20:44 PDT
Magnitude6.0 M_w
Depth11.3 km
LocationNapa County, California
TypeStrike-slip
AffectedNapa County, Sonoma County, San Francisco Bay Area
IntensityVII–VIII (Modified Mercalli)

2017 Napa earthquake

The August 24, 2017 seismic event struck northern California near the city of Napa, producing strong ground shaking across the San Francisco Bay Area, damage in Napa County, California, and aftershocks felt as far as Sacramento, California and San Jose, California. The rupture occurred on a previously mapped but incompletely characterized fault zone adjacent to the Calaveras Fault and Hayward Fault, generating a moment magnitude of 6.0 and a focal depth of about 11 km. Scientists from the United States Geological Survey, California Geological Survey, and academic institutions mobilized to document the sequence, while local, state, and federal agencies coordinated emergency response and recovery.

Background and tectonic setting

The northern California region lies within the complex plate boundary between the Pacific Plate and the North American Plate, where the relative motion is accommodated by the San Andreas Fault system, including subsidiary structures such as the Hayward Fault Zone, Calaveras Fault, and the Rodgers Creek Fault. The Napa epicentral area is crossed by the Napa and West Napa fault strands, which had been identified by studies from the United States Geological Survey and the California Geological Survey but lacked detailed paleoseismic records comparable to the Hayward Fault trench studies. Historical seismicity in the region includes the 1989 Loma Prieta earthquake and numerous smaller events catalogued by the National Earthquake Information Center. Geologic mapping by the United States Geological Survey and paleoseismology teams from Stanford University and the University of California, Berkeley had highlighted complex fault interactions in the northern San Pablo Bay and Sonoma County, California area.

Earthquake sequence and characteristics

The mainshock, recorded at 10:20:44 PDT, was a right-lateral strike-slip event with a moment magnitude of 6.0 as reported by the United States Geological Survey and the Global Centroid Moment Tensor Project. The rupture propagated on a northwest–southeast trending fault near the city of Napa, producing surface fissures and measurable offsets documented by field teams from USGS, California Institute of Technology, and the University of California, Davis. Seismograms from regional networks including the Berkeley Seismological Laboratory and the Southern California Seismic Network recorded strong high-frequency energy typical of shallow crustal earthquakes. The mainshock was followed by an aftershock sequence that included multiple events greater than magnitude 4.0, catalogued and analyzed by the National Seismic Network and researchers at Scripps Institution of Oceanography.

Damage and casualties

The event produced structural and nonstructural damage across Napa, California, Sonoma County, California, and parts of the San Francisco, Oakland, California, and San Rafael, California metropolitan areas. Historical landmarks such as buildings in the Napa County Courthouse complex and commercial properties on First Street, Napa sustained damage, prompting assessments by teams from the California Office of Emergency Services and the National Park Service for registered historic structures. Industrial facilities including wineries and manufacturing sites reported broken tanks and items, while hospitals such as Queen of the Valley Medical Center activated emergency procedures. The shaking led to roof collapses, cracked masonry, and chimney failures in numerous California Historical Landmarks, with inspectors from the California Office of Historic Preservation and structural engineers from the American Society of Civil Engineers evaluating safety. Several dozen injuries were treated at local hospitals; there were a small number of fatalities associated with the event reported by the Napa County Sheriff's Office and the California Highway Patrol during the immediate aftermath.

Response and recovery

Local emergency management agencies including the Napa County Office of Emergency Services and the City of Napa, California emergency operations center initiated search and rescue, damage assessment, and public information campaigns. The California Governor's Office coordinated state resources and activated mutual aid through the California Office of Emergency Services, while the Federal Emergency Management Agency provided technical assistance and disaster recovery guidance. Utilities such as Pacific Gas and Electric Company conducted rapid inspections of gas and electrical infrastructure, and transit agencies including the Bay Area Rapid Transit and California Department of Transportation inspected tracks and bridges. Nonprofit organizations like the American Red Cross and community groups mobilized shelters and aid; academic teams from University of California, Berkeley and Stanford University deployed rapid post-earthquake reconnaissance, contributing to engineering reports published by the Earthquake Engineering Research Institute.

Impact on infrastructure and economy

The earthquake disrupted transportation corridors managed by the California Department of Transportation and local transit providers, with damage to roadways on California State Route 12 and temporary closures on segments of U.S. Route 101 for inspections. Utility outages affected customers of Pacific Gas and Electric Company and water delivery systems overseen by the Napa Sanitation District until repairs were completed. The event inflicted economic losses to the regional wine industry centered in Napa Valley, with damage to wineries, storage tanks, and retail venues; insurers including the California Earthquake Authority processed numerous claims, and economic impact assessments were prepared by regional chambers such as the Napa Valley Vintners and the Napa Chamber of Commerce. Longer-term resilience investments were informed by reports from the United States Geological Survey, the Federal Emergency Management Agency, and the National Institute of Standards and Technology, influencing seismic retrofitting priorities for historic buildings, transportation assets, and utility infrastructure.

Category:2017 earthquakes Category:Earthquakes in California Category:Napa County, California