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When tectonic plates shift and energy is released, it can result in an earthquake. The released energy causes seismic waves to travel through the Earth, leading to ground shaking and potential damage to infrastructure and property. The intensity of the earthquake depends on factors such as the magnitude of the energy release and the proximity to populated areas.
The movement of tectonic plates is primarily driven by the energy released from the Earth's internal heat, known as geothermal energy. This energy causes convection currents in the mantle, which in turn exerts forces on the tectonic plates, causing them to move.
friction
Earthquakes are a feature associated with colliding plates. When tectonic plates collide, the intense pressure and friction can cause the plates to stick and build up stress. When this stress is released suddenly, it results in seismic energy being released in the form of an earthquake.
They are called tectonic or lithospheric plates.
Earthquakes are caused by the movement of tectonic plates beneath the Earth's surface. When these plates shift, it can release energy in the form of seismic waves, resulting in the ground shaking. The magnitude of an earthquake is determined by the amount of energy released during this movement.