Martian Araneiforms: A Review

Araneiforms are enigmatic dendritic negative topography features native to Mars. Found across a variety of substrates and exhibiting a range of scales, morphologies, and activity level, they are hypothesized to form via insolation‐induced basal sublimation of seasonal CO2 ice. With no direct Earth a...

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Veröffentlicht in:	Journal of geophysical research. Planets 2023-04, Vol.128 (4), p.n/a
Hauptverfasser:	Mc Keown, L. E., Diniega, S., Portyankina, G., Hansen, C. J., Aye, K.‐M., Piqueux, S., Scully, J. E. C.
Format:	Artikel
Sprache:	eng
Schlagworte:	Carbon dioxide CO2 sublimation Earth Earth analogs Ice Image resolution Laboratories Mars Mars seasonal processes Mars surface Martian araneiforms Martian spiders planetary geomorphology Planetary surfaces Planetology Polar environments Polar regions Questions Regolith Seasonal variations Sublimation Substrates Sunlight the Kieffer model Troughs
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