What type of fault is the San Andreas Fault in California?
strike-slip fault
what type of fault is the San Andreas? A San Andreas earthquake would be classified as occurring on a strike-slip fault. Strike-slip faults are found along boundaries of tectonic plates sliding past each other.
Is the San Andreas Fault in California is an example of a transform plate boundary?
The San Andreas Fault is the transform plate boundary where a thin sliver of western California, as part of the Pacific Plate, slides north-northwestward past the rest of North America.
What is the San Andreas Fault and example of?
The San Andreas Fault is a continental transform fault that extends roughly 1,200 kilometers (750 mi) through California. It forms the tectonic boundary between the Pacific Plate and the North American Plate, and its motion is right-lateral strike-slip (horizontal).
Is California’s San Andreas Fault a dip slip fault?
The Northern Pacific plate is sliding laterally past the North American plate in a northerly direction, and hence the San Andreas is classified as a strike-slip fault.
Can the San Andreas fault cause a tsunami?
Tsunamis can be caused by a variety of events, including landslides, volcanic activity and most commonly, earthquakes. Quakes along strike-slip faults like the San Andreas, in which two plates slide past one another, weren’t thought to cause tsunamis on their own because they cause largely horizontal motion.
Why is San Andreas fault so dangerous?
Narrator: Parts of the San Andreas Fault intersect with 39 gas and oil pipelines. This could rupture high-pressure gas lines, releasing gas into the air and igniting potentially deadly explosions. Stewart: So, if you have natural-gas lines that rupture, that’s how you can get fire and explosions.
What kind of fault is the San Andreas Fault?
San Andreas Fault. The San Andreas Fault is a continental transform fault that extends roughly 1,200 kilometers (750 mi) through California. It forms the tectonic boundary between the Pacific Plate and the North American Plate, and its motion is right-lateral strike-slip (horizontal).
Who was the geologist who discovered the San Andreas Fault?
In 1953, geologist Thomas Dibblee concluded that hundreds of miles of lateral movement could occur along the fault.
Where are the Red rhombs on the San Andreas Fault?
The red rhombs are pull-apart basins; the northern one is the site of the Niland geothermal field, the southern the Cerro Prieto geothermal field. The Vasquez Rocks in Agua Dulce, California are evidence of the San Andreas Fault and part of the 2,650-mile Pacific Crest Trail.
Where was the San Andreas Fault observatory located?
A project called the San Andreas Fault Observatory at Depth (SAFOD) near Parkfield, Monterey County, was drilled through the fault during 2004–2007 to collect material and make physical and chemical observations to better understand fault behavior.