The formation of gullies on Mars today

Colin M. Dundas, Alfred S. McEwen, Serina Diniega, Candice J. Hansen, Shane Byrne, Jim N. McElwaine

Research output: Contribution to journalArticle

17 Scopus citations

Abstract

A decade of high-resolution monitoring has revealed extensive activity in fresh Martian gullies. Flows within the gullies are diverse: They can be relatively light, neutral or dark, colourful or bland, and range from superficial deposits to 10 m-scale topographic changes. We observed erosion and transport of material within gullies, new terraces, freshly eroded channel segments, migrating sinuous curves, channel abandonment, and lobate deposits. We also observed early stages of gully initiation, demonstrating that these processes are not merely modifying pre-existing landforms. The timing of activity closely correlates with the presence of seasonal CO 2 frost, so the current changes must be part of ongoing gully formation that is driven largely by its presence. We suggest that the cumulative effect of many flows erodes alcoves and channels, and builds lobate aprons, with no involvement of liquid water. Instead, flows may be fluidized by sublimation of entrained CO 2 ice or other mechanisms. The frequent activity is likely to have erased any features dating from high-obliquity periods, so fresh gully geomorphology at middle and high latitudes is not evidence for past liquid water. CO 2 ice-driven processes may have been important throughout Martian geological history and their deposits could exist in the rock record, perhaps resembling debris-flow sediments.

Original languageEnglish (US)
Pages (from-to)67-94
Number of pages28
JournalGeological Society Special Publication
Volume467
Issue number1
DOIs
StatePublished - 2019

ASJC Scopus subject areas

  • Water Science and Technology
  • Ocean Engineering
  • Geology

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    Dundas, C. M., McEwen, A. S., Diniega, S., Hansen, C. J., Byrne, S., & McElwaine, J. N. (2019). The formation of gullies on Mars today. Geological Society Special Publication, 467(1), 67-94. https://doi.org/10.1144/SP467.5