BIROn - Birkbeck Institutional Research Online

    Episodic and declining fluvial processes in Southwest Melas Chasma, Valles Marineris, Mars

    Davis, Joel and Grindrod, Peter and Fawdon, Peter and Williams, R.M.E. and Gupta, S. and Balme, M. (2018) Episodic and declining fluvial processes in Southwest Melas Chasma, Valles Marineris, Mars. Journal of Geophysical Research: Planets 123 (10), pp. 2527-2549. ISSN 2169-9097.

    [img]
    Preview
    Text
    49990.pdf - Published Version of Record
    Available under License Creative Commons Attribution.

    Download (6MB) | Preview

    Abstract

    There is abundant evidence for aqueous processes on Noachian terrains across Mars; however, key questions remain about whether these processes continued into the Hesperian as the martian climate became less temperate. One region with an extensive Hesperian sedimentary record is Valles Marineris. We use high-resolution image and topographic data sets to investigate the fluvial systems in the southwest Melas basin, Valles Marineris, Mars. Fluvial landforms in the basin exist across a wide area, and some are preserved as inverted channels. The stratigraphy of the basin is complex: Fluvial landforms are preserved as planview geomorphic features and are also interbedded with layered deposits in the basin. The fluvial morphologies are consistent with formation by precipitation-driven runoff. Fluvial processes in the basin were episodic, suggesting multiple wet and dry periods. During dry periods, mantling material accumulated, and significant volumes of sediment were eroded, inverting fluvial channels. During wet periods, inverted channels and mantling material infilling valleys were incised by further fluvial erosion. These trends for episodic fluvial processes are similarly reflected in the central depression of the southwest Melas basin, previously described as a paleolake. Ultimately, fluvial processes in the basin gradually shut down, becoming geographically restricted, and then ceased entirely. We show that branching valley networks are also present on the plateaus above Melas and Ius Chasma, which converge on the heads of tributary canyons. These suggest that precipitation-driven runoff processes also extended onto the plateaus of Valles Marineris.

    Metadata

    Item Type: Article
    School: Birkbeck Faculties and Schools > Faculty of Science > School of Natural Sciences
    Depositing User: Joel Davis
    Date Deposited: 28 Nov 2022 16:51
    Last Modified: 02 Aug 2023 18:19
    URI: https://eprints.bbk.ac.uk/id/eprint/49990

    Statistics

    Activity Overview
    6 month trend
    37Downloads
    6 month trend
    69Hits

    Additional statistics are available via IRStats2.

    Archive Staff Only (login required)

    Edit/View Item
    Edit/View Item