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The tsunami that struck Thailand on December 26, 2004, was caused by a massive earthquake with a magnitude of 9.1 to 9.3 on the Richter scale. The epicenter of the earthquake was located off the west coast of northern Sumatra, Indonesia. The earthquake was caused by the Indian and Australian tectonic plates moving against each other, resulting in a large-scale displacement of water. This displacement created a series of massive waves that traveled at high speeds across the Indian Ocean, eventual
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Steller Sphere on Instagram: "Tectonic plates cause tsunamis primarily through underwater earthquakes at subduction zones, where one plate dives beneath another. These collisions cause the seafloor to suddenly shift upward or downward, displacing massive volumes of water, which generates fast-moving, high-energy waves that travel across the ocean and swell into devastating surges upon reaching shallow coastal waters. Key aspects of how tectonic plates generate tsunamis include: • Subduction Zone
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