yes, they can
False. Earthquakes mostly occur along faults that are at or very near to plate boundaries.
They usually occur in places where two plates meet- faults.
Yes, but not as often as earthquakes happen near plate boundaries
yes
Earthquakes occur along faults because faults are cracks in the Earth's surface where tectonic plates interact. When stress builds up along a fault line and is released suddenly, it causes rocks to break and shift, resulting in an earthquake. The movement of the tectonic plates along faults is what ultimately causes earthquakes to happen.
Intraplate earthquakes occur farther inland than other earthquakes. These earthquakes occur within a tectonic plate, away from plate boundaries where most earthquakes typically occur. Intraplate earthquakes can be caused by ancient faults or stress within the plate itself.
Not necessarily. Earthquakes occur when there is movement along cracks in the Earth's crust called faults. There are three main types of fault, all of which can produce earthquakes. Normal faults usually occur where the crust is being pulled apart. Reverse faults, also called thrust faults, are usually found where sections of the crust are pushed together. Transform faults occur where sections of the crust slide past each other horizontally, neither pushing together nor pulling apart.
Earthquakes infrequently occur away from plate boundaries. Most earthquakes occur at plate boundaries because of the stress caused by the interacting plates.
Because it is a fault and earthquakes usually occur near faults.
Most earthquakes occur near faults because the interaction of tectonic plates (moving against or away from each other) causes a buildup of stress, which is eventually released in the form of an earthquake. Earthquakes don't necessarily occur along faults though. Volcanic activity and isostatic imbalance (local imbalance from rapid geologic change - for example, ice melting) are two other causes of earthquakes.
near subduction zones
Not all motion along large faults results in destructive earthquakes. Some faults experience slow, steady movement known as creep, which releases stress gradually and may not generate significant shaking. In contrast, earthquakes occur when accumulated stress is suddenly released along a fault, leading to rapid movement and seismic waves.