they are making earthquakes
The San Andreas fault lies along a transform fault line where two of the Earth's plates are sliding past each other. At San Andreas, the Pacific Plate (to the west) slides past the North American Plate (to the east).
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Earthquakes occur along the San Andreas Fault because of the tectonic plates. When the plates slip or shift, an earthquake happens.
sliding up next to each other causing earthquakes
The San Andreas Fault is a transform fault boundary where two tectonic plates, the Pacific Plate and the North American Plate, meet. These plates are moving horizontally past each other. As a result, the motion along the fault can cause earthquakes due to the stress and friction as the plates grind against each other.
it was caused by the two plates in the earth that hit each other
Yes, the San Andreas Fault is a transform fault boundary separating the Pacific Plate and the North American Plate. Stress along this boundary causes earthquakes as the plates slide past each other horizontally.
The ridges and cracks along the San Andreas Fault are a result of the movement of tectonic plates. The fault marks the boundary between two plates that are slowly sliding past each other, causing stress to build up and be released in the form of earthquakes. Over time, this movement creates the ridges and cracks that we see along the fault line.
The two continental plates that meet at the San Andreas Fault are the North American Plate and the Pacific Plate. These plates are moving horizontally past each other, which causes a lot of seismic activity along the fault line. The movement has led to numerous earthquakes in California, making the San Andreas Fault one of the most well-known geological features in the world.
AnswerAccording to the USGS, the plates along the San Andrea fault move about 1.7in per year.
Volcanoes do not form along the San Andreas Fault because the fault is a transform boundary where two tectonic plates slide past each other horizontally, rather than colliding or separating to create the conditions necessary for volcanic activity.
In plate tectonics, a sliding boundary is considered a transform fault where the two merging plates slide past each other in the opposite direction. A great example of a transform fault would be in California along the San Andreas fault line.