Young Valley Networks on Mars: Persistent Flow of Water in Lyot Crater, an Amazonian Impact Basin Microenvironment

Physics

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Scientific paper

We document a suite of sinuous valley networks on the floor of Lyot
Crater that incise a mantling unit dated as mid-Amazonian. We interpret
the valley networks to be fluvial in origin and to have been sourced by
mid- or late-Amazonian glacial units.

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