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Showing 1–3 of 3 results

Advanced filters: Author: Jan Raack Clear advanced filters

Water induced sediment levitation enhances downslope transport on Mars

Downslope sediment transport on Mars is reported, but the transport capacity of unstable water under low pressures is not well understood. Here, the authors present a newly discovered, highly reactive transportation mechanism that is only possible under low pressure environments.

Jan Raack
Susan J. Conway
Manish R. Patel
ResearchOpen Access27 Oct 2017
Nature Communications

Volume: 8, P: 1-10
Experimental evidence for lava-like mud flows under Martian surface conditions

Experimental mudflows under Martian surface conditions propagate similarly to terrestrial pahoehoe lava flows, suggesting mud (rather than igneous) volcanism can explain some flow morphologies on Mars.

Petr Brož
Ondřej Krýza
Manish R. Patel
Research18 May 2020
Nature Geoscience

Volume: 13, P: 403-407
How, when and where current mass flows in Martian gullies are driven by CO₂ sublimation

Carbon dioxide gas sublimated from frost at locations of high temperature difference could mobilize surface sediments in gully features observed on the Martian surface, according to flume tank experiments and numerical climate modelling.

Lonneke Roelofs
Susan J. Conway
Manish R. Patel
ResearchOpen Access13 Mar 2024
Communications Earth & Environment

Volume: 5, P: 1-9