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C. Clark

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Open access Aug 2026

Amazonian-aged glacial melting recorded by a subglacial paleolake and regionally widespread eskers on Mars

The mid-to-late Amazonian period on Mars (ca. 0−1 Ga) was cold and hyperarid, with an extremely limited role of liquid water. Abundant midlatitude viscous flow features (VFFs; putative debris-covered glaciers) that formed during this time are thought to be the partially retreated remnants of larger, thicker, predominan...

F. Butcher, N. Arnold, A. Johnsson et al. · 0 citations

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