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Shock-heating in geophysics refers to the intense heating that occurs during the impact of celestial bodies, such as meteorites, with planets or moons. When an object strikes a planetary surface at hypervelocity speeds, it releases a tremendous amount of kinetic energy, similar to a nuclear explosion. This impact generates powerful shock waves that penetrate the surface, vaporizing, melting, and crushing material.123

The debris from the impact can then blanket the planet's surface, trapping heat and potentially causing the planet to melt. This process is a significant factor in the early development and geological history of planets, including Earth, and is responsible for the formation of meteorite craters.12

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