Tongue Ridges and Rumpled Crater Floors in Mid-Southern-Latitude Martian Craters

Physics

Scientific paper

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Scientific paper

Mid-southern latitude craters on Mars exhibit tongue-like ridges
extending from the base of south-facing crater walls that enclose
smooth, concave floors. These form from retreat of gullied ice fans and
massive ice deposits. The ice forces inward flow of ice-rich crater
floor deposits.

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