The Sublimation and Relaxation of Troughs and Scarps Within the Martian North Polar Layered Deposits

Mathematics – Logic

Scientific paper

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Scientific paper

Although the morphological evolution of the NPLD is widely presumed to
result from surface ablational processes, we show that viscous
relaxation of subsurface water ice is more consistent with the slope and
depth distributions of NPLD troughs and scarps.

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