It's a earthquake where two plates move sideways from eachother for example the San Andreas Fault is a strike-slip earthquake.
Move away from a fault line.
Parts of it will end up further North.
California has earth quakes because it is on plates under neath the earth once the plates move the ground shakes. Its kind of like Haiti. Its right were the tectonic plates move and because of convection currents and other things the earth spreads a part from eachother, like how we were in Pangaea.
when did this particular fualt last move
The San Andreas Fault is a result of the tectonic forces causing the Pacific Plate to move northwestward relative to the North American Plate. This movement creates significant stresses that are relieved through periodic earthquakes along the fault line.
The San Andreas fault is a strike-slip fault, where two tectonic plates move horizontally past each other. It is not a reverse fault, where the hanging wall moves up relative to the footwall due to compression.
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.
It's a earthquake where two plates move sideways from eachother for example the San Andreas Fault is a strike-slip earthquake.
This is a strike-slip fault.
Move away from a fault line.
The most common type of fault in the northern San Andreas Fault system is strike-slip fault, where the blocks move horizontally past each other. This fault system is characterized by lateral movement along the fault line, with the Pacific Plate moving northwest relative to the North American Plate.
The San Andreas Fault is a strike-slip fault, where two tectonic plates move horizontally past each other. The main force causing movement along the fault is the tectonic forces generated by the motion of the Pacific Plate relative to the North American Plate.
AnswerAccording to the USGS, the plates along the San Andrea fault move about 1.7in per year.
The most common type of fault is a strike-slip fault, where two blocks of rock move horizontally past each other. This type of fault is often associated with transform plate boundaries, such as the San Andreas Fault in California.
When rocks on either side of a fault move in different directions, it is known as a strike-slip fault. This type of fault occurs when the rocks slide past each other horizontally. Examples of strike-slip faults include the San Andreas Fault in California.
The Christchurch fault line last moved on monday 13/03/13 at 7 pm. Eva is cool