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Strike Slip/Transform. Like the San Andreas Fault in California.
the shaking of the earthquake
transform fault boundary
The plates have changed because of age and when the plates move they grind.
Transform fault boundaries happen at the site where two tectonic plates move past each other in opposite directions. The two plates will grind past each other, breaking off pieces of crust from the plates. The plates can get caught on each other and pressure will build up until a break develops and the plates will lurch forward.
transform fault boundary
transform fault boundary
The San Andreas Fault in California, where the Pacific Plate meets the North American Plate and they grind past each other. Also: Turkey's North Anatolian Fault New Zealand's Alpine Fault
Sacramento, California is on the North American Plate near the boundary with the Pacific Plate. As these plates grind against each other it creates earthquakes that can affect the area.
tetoic plates grind the grind a slip past each other
California sits along the San Andreas Fault. Here, two slabs of Earth's crust, called tectonic plates, slowly grind past one another. As this happens the plates snag on one another and build up tension. Every so often the plates slip and this tension is released in the form of earthquakes.
with a screwdriver