The Open UniversitySkip to content

Present-day development of gully-channel sinuosity by carbon dioxide gas supported flows on Mars

Pasquon, Kelly; Gargani, Julien; Massé, Marion; Vincendon, Mathieu; Conway, Susan J.; Séjourné, Antoine; Jomelli, Vincent; Balme, Matthew; Lopez, Simon and Guimpier, Anthony (2019). Present-day development of gully-channel sinuosity by carbon dioxide gas supported flows on Mars. Icarus, 329 pp. 296–313.

DOI (Digital Object Identifier) Link:
Google Scholar: Look up in Google Scholar


Martian gullies have been widely studied, but their formation mechanism is still under debate. Their channels generally trend straight downslope, but some display sinuosity. Seasonally active gullies are common on sand dunes and their channels have been reported to develop sinuosity. Here, we perform a detailed analysis of a gully on a dune within Matara Crater (49.5°S; 34.9°E) where development of channel sinuosity has taken place over 5 martian years (MY29-33) of observation. This study was performed using HiRISE images, HiRISE elevation data, spectroscopic CRISM data and a 1D GCM for surface temperature modelling. The morphological evolution of the gully suggests a significant seasonal contribution of fluid. Each year we observed material collapse and accumulation in the alcove, followed by transport events during which lateral migration and extension of the channel occur together with growth of the debris apron. Over one martian year, the debris apron propagated by almost 140 m from an initial length of 800 m. These transport events occur in the middle of winter when CO2 frost is still present and are contemporaneous with the beginning of the defrosting. We propose that the activity and the sinuosity development in the gully could be explained by: 1) a flow composed of sand and CO2 gas, producing morphologies similar to those in hyper-concentrated flows on Earth and 2) contribution of material from alternating of the alcove source location.

Item Type: Journal Item
Copyright Holders: 2019 Elsevier Inc.
ISSN: 0019-1035
Keywords: Mars; Mars surface; Mars climate; Geological processes; Ices
Academic Unit/School: Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
Item ID: 61231
Depositing User: ORO Import
Date Deposited: 15 May 2019 13:26
Last Modified: 09 Dec 2019 14:40
Share this page:


Altmetrics from Altmetric

Citations from Dimensions

Actions (login may be required)

Policies | Disclaimer

© The Open University   contact the OU