Insight to the Evolution of Wrinkle Ridges in Hesperia Planum, Mars

Physics

Scientific paper

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Scientific paper

Wrinkle ridges are linear to arcuate, asymmetric, topographic highs; the
precise origin is unknown. Study results reveal NE-striking wrinkle
ridges formed prior to NW-striking wrinkle ridges, and the deposits of
Hesperia Planum are thin, <2km.

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