An earthquake typically occurs as a result of divergent, convergent, or remodelling in the plate, and it is capable of causing tsunamis due to its precise state.
An earthquake (additionally referred to as a quake, tremor, or temblor) is the shaking of the floor of the Earth because of an unexpected launch of power within the Earth's lithosphere that creates seismic waves.
Earthquakes can range in length from those that are so weak that they cannot be felt to those that are powerful enough to propel objects and people into the air and wreak havoc on entire cities.
The seismicity, or seismic activity, of a place is the frequency, type, and length of earthquakes experienced over a selected time period. The phrase "tremor" is likewise used for non-earthquake seismic rumbling.
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