The average amount of diplacement along the San Andreas Fault is 2 to 5 centimeters (1 to 2 inches) per year.
No, the San Andreas Fault does not have any volcanoes along its path.
AnswerAccording to the USGS, the plates along the San Andrea fault move about 1.7in per year.
It is a transform fault where rocks on either side of the fault move sideways past each other. This motion is caused by shearing forces that result in horizontal displacement along the fault line. Examples of transform faults include the San Andreas Fault in California.
On average, the San Andreas Fault experiences thousands of small earthquakes every year, but only a few are typically felt by people. The fault system is seismically active due to the movement of the North American and Pacific tectonic plates along this boundary.
The San Andreas Fault is a transform boundary where the Pacific Plate and the North American Plate are sliding past each other horizontally. The relative movement along the fault is primarily strike-slip, with occasional vertical movement during earthquakes.
No the time-scales for that sort of displacement along the San Andreas fault are on the order of millions of years not decades.
No, the San Andreas Fault does not have any volcanoes along its path.
The San Andreas fault is where it occured.
The offset along a fault is the distance by which one side of the fault has moved in relation to the other side. This movement can be horizontal, vertical, or a combination of both, and it is a measure of the displacement that has taken place along the fault.
Earthquakes occur along a fault. Near the San Andreas fault lots of earthquakes occur.
If the fault is responsible for the earthquake, there will be movement (displacement) along the fault.
If the fault is responsible for the earthquake, there will be movement (displacement) along the fault.
AnswerAccording to the USGS, the plates along the San Andrea fault move about 1.7in per year.
they are making earthquakes
Along the San Andreas Fault line.
It is a transform fault where rocks on either side of the fault move sideways past each other. This motion is caused by shearing forces that result in horizontal displacement along the fault line. Examples of transform faults include the San Andreas Fault in California.
If the fault is responsible for the earthquake, there will be movement (displacement) along the fault.