Liquefaction occurs when intense shaking causes the water pressure between soil particles to increase. This causes the soil to lose its strength and act like a liquid. Buildings on such soil may tilt, sink or collapse as the foundation literally ...
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The Wadati-Benioff Zone is a dipping area of earthquake foci that tracks the path of a subducting tectonic plate as it sinks into the mantle. It can extend to depths of up to 700 km. It provides visual evidence that ...
Love waves (L-waves) are surface waves that move the ground in a horizontal, shearing motion. They do not have a vertical component. This side-to-side shaking is particularly destructive to buildings because most structures are designed to handle vertical gravity loads ...
P-waves slow down significantly when entering the liquid outer core from the solid mantle. This sudden velocity drop causes the waves to bend (refract) toward the center of the Earth. This bending creates a “gap” on the surface between 103° ...
Earthquakes on the eastern margins of Asia (Japan, Kuril Islands, Philippines) are primarily caused by the subduction of the Pacific Plate beneath the Asian (Eurasian) Plate. As the heavy oceanic Pacific Plate sinks into the mantle, it creates a massive ...