The movement and interaction of tectonic plates is the primary cause of earthquakes, volcanic eruptions, and the formation of mountains and ocean basins. When these plates collide or slide against each other, they can generate intense pressure and friction, which eventually leads to seismic activity and the release of energy in the form of earthquakes. Volcanic eruptions occur when molten rock, called magma, rises to the surface through cracks and openings in the Earth's crust. This can happen due to the movement and interaction of tectonic plates or when the pressure of trapped gases within the magma becomes too high. The convergence or divergence of tectonic plates also influences the creation of mountains and ocean basins. When two plates collide, they can form large uplifted areas that eventually become mountains. In contrast, when two plates move apart, they create a gap or rift that can fill with water, forming an ocean basin.
