|
instanceOf
|
geological fault
→
plate boundary
→
strike-slip fault
→
transform fault
→
|
|
averageSlipRate
|
about 20 to 35 millimeters per year
→
|
|
country
|
United States
→
|
|
cumulativeOffset
|
hundreds of kilometers over millions of years
→
|
|
discoveredBy
|
Andrew Lawson
→
|
|
discoveryYear
|
1895
→
|
|
formsBoundaryOf
|
North American Plate western margin in California
→
|
|
geologicalAge
|
tens of millions of years
→
|
|
governedBy
|
plate tectonics
→
|
|
hasFeature
|
fault scarps
→
linear valleys
→
offset streams
→
|
|
hazardType
|
large earthquakes
→
|
|
length
|
about 1200 kilometers
→
about 750 miles
→
|
|
locatedIn
|
California
→
western United States
→
|
|
maximumObservedOffset
|
several meters in single events
→
|
|
monitoredBy
|
United States Geological Survey
→
|
|
namedAfter
|
San Andreas Lake
→
|
|
notableEarthquake
|
1857 Fort Tejon earthquake
→
1906 San Francisco earthquake
→
1989 Loma Prieta earthquake
→
|
|
orientation
|
northwest–southeast
→
|
|
partOf
|
Pacific Ring of Fire
→
|
|
passesNear
|
Los Angeles
→
San Francisco
→
|
|
passesThrough
|
Carrizo Plain
→
Coachella Valley
→
Mojave Desert region
→
Salton Sea region
→
San Bernardino Mountains region
→
San Francisco Peninsula
→
|
|
region
|
California Coast Ranges
→
Peninsular Ranges
→
Transverse Ranges
→
|
|
relativeMotionType
|
right-lateral strike-slip
→
|
|
riskTo
|
Greater Los Angeles area
→
San Francisco Bay Area
→
|
|
segment
|
central segment
→
northern segment
→
southern segment
→
|
|
seismicZone
|
San Andreas Fault system
→
|
|
tectonicPlateBoundaryBetween
|
North American Plate
→
Pacific Plate
→
|
|
terminusNear
|
Cape Mendocino
→
Salton Sea
→
|