Construct · 1 fields · 1 citations
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In planetary science a crater is the bowl-shaped scar left when a meteoroid or asteroid strikes a surface at high speed, the kinetic energy of the impact excavating and ejecting rock and often leaving a raised rim and central peak. Crater size and form record the energy of the impact and the age of the surface, since older terrains accumulate more craters. Melosh's Impact Cratering: A Geologic Process is the standard treatment of the shock physics and resulting landforms. The referent is an excavation formed by impact, measured by diameter, depth, and morphology, distinct from a vent in a volcano or a pit at the end of a weld.[1]
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