Hayward Fault

E96858

The Hayward Fault is a major geologic fault in the San Francisco Bay Area known for its high seismic risk and potential to generate powerful earthquakes.


Statements (49)
Predicate Object
instanceOf geologic fault
right-lateral fault
strike-slip fault
causes ground rupture
surface creep
cityMostAtRisk Berkeley, California NERFINISHED
Fremont, California
Hayward, California
Oakland, California NERFINISHED
connectedTo Rodgers Creek Fault
country United States
hazardTo critical infrastructure in the East Bay
hazardType earthquake
surface fault rupture
includedIn USGS National Seismic Hazard Model
knownFor high seismic hazard
potential to generate powerful earthquakes
lastMajorEarthquakeMagnitudeApprox 6.8–7.0
lastMajorEarthquakeName 1868 Hayward earthquake
lastMajorEarthquakeYear 1868
lengthApproxKm ~119
locatedIn Northern California
San Francisco Bay Area
monitoredBy California Geological Survey
United States Geological Survey
near San Francisco, California
notableEvent 1868 Hayward earthquake
observedPhenomenon aseismic creep
orientationGeneral northwest–southeast
parallelTo San Andreas Fault
partOf San Andreas Fault system
passesUnder California Memorial Stadium
University of California, Berkeley campus
plateOnEastSide North American Plate
plateOnWestSide Pacific Plate
recurrenceIntervalEstimateYears ~140
regionPopulationExposed millions of people
relativeMotion right-lateral strike-slip
runsThrough Berkeley, California
East Bay
Fremont, California
Hayward, California
Oakland, California NERFINISHED
San Leandro, California
Union City, California
segmentOf Hayward–Rodgers Creek fault zone
seismicRiskLevel high
slipRateApproxMmPerYear ~9
tectonicSetting transform plate boundary

Referenced by (2)
Subject (surface form when different) Predicate
California Memorial Stadium
builtNear
Hayward Fault ("Hayward–Rodgers Creek fault zone")
segmentOf

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