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The Earth's outer layer, the lithosphere, is made up of several large and small plates called tectonic plates. These plates are constantly moving, albeit very slowly, on the semi-fluid asthenosphere below. The movement of these plates is the primary cause of **earthquakes**. They can collide, slide past each other, or move apart. The boundaries of these plates are where most **earthquakes** occur. Areas along these boundaries, like the infamous Ring of Fire, are prone to regular seismic activity. As the plates move, they build up stress. When this stress exceeds the strength of the rocks, the rocks suddenly break, releasing energy in the form of seismic waves. This sudden release of energy is what we feel as an **earthquake**.
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