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Identification of gully debris flow deposits in Protonilus Mensae, Mars: Characterization of a water-bearing, energetic gully-forming process

Levy, J. S. and Head, J. W. and Dickson, J. L. and Fassett, C. I. and Morgan, G. A. and Schon, S. C. (2010) Identification of gully debris flow deposits in Protonilus Mensae, Mars: Characterization of a water-bearing, energetic gully-forming process. Earth and Planetary Science Letters, 294 (3-4). pp. 368-377. ISSN 0012-821X. https://resolver.caltech.edu/CaltechAUTHORS:20161130-111347377

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Abstract

Gullies are a class of geologically recent landform on Mars that show evidence of downslope transport of sedimentary material from recessed alcoves, through incised channels, to distributary fans or aprons. The mechanisms invoked to account for the formation of gullies on Mars range from completely dry, granular flows or landslides, to debris flows that incorporate some component of liquid water, to fluvial erosion and alluvial-fan-like deposition. Each of these processes requires different amounts of liquid water, and produces different characteristic morphologies. We report on the identification of unusual lobate structures present in proximity to gullies in Protonilus Mensae. The lobes are up to ~ 3 m thick and terminate in rounded snouts. These lobate structures are present mostly downslope of gullies, and can be traced upslope through channels, to gully fan termini, and in places, onto gully fan surfaces. Crater dating indicates that the deposits formed recently—potentially within the past ~ 500 ka. We use HRSC digital elevation models to constrain mechanical properties of the lobate deposits, and to compare their formation environment to that of typical martian gullies. The Protonilus Mensae lobate deposits are interpreted to indicate local dominance of wet debris flows in the formation of the observed gullies and lobes. These observations are consistent with 1) top-down melting of the ice component of the latitude-dependent mantle terrain in which the gullies form and 2) initiation of debris flows by mobilization of the dusty lithic component of the mantle. The suite of morphological observations diagnostic of wet debris flow processes suggests the identification of an unusual environment in which the wet debris-flow formational end-member is locally the dominant gully forming process; elsewhere on Mars gully morphology may be more consistent with a range of other water-related sediment transport mechanisms including fluvial erosion, hyperconcentrated flow, and low-strength mudflows (that deposit as fans rather than lobes). These results suggest that 1) gully-forming processes involve liquid water, 2) that the water source is associated with the martian latitude-dependent mantle, and 3) that a range of water-related sediment transport processes is involved in gully formation.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/j.epsl.2009.08.002DOIArticle
http://www.sciencedirect.com/science/article/pii/S0012821X09004580PublisherArticle
ORCID:
AuthorORCID
Head, J. W.0000-0003-2013-560X
Fassett, C. I.0000-0001-9155-3804
Additional Information:© 2009 Elsevier B.V. Accepted 4 August 2009; Available online 31 August 2009. We gratefully acknowledge support from the Mars Exploration Program Mars Express HRSC grant JPL 1237163, and the Mars Data Analysis Program grants NNG05GQ46G and NNX07AN95G to JWH. Thanks to the HiRISE and CTX teams for use of high-resolution image data, and to the Mars Express HRSC team for production of high-quality digital elevation models. Thanks to John Huffman for assistance in stereo image processing and visualization, and to the NASA AISR program for support of data visualization and analysis (NNX08AC63G).
Funders:
Funding AgencyGrant Number
JPL1237163
NASANNG05GQ46G
NASANNX07AN95G
NASANNX08AC63G
Subject Keywords:Mars; gully; pasted-on terrain; permafrost; debris flow; climate
Issue or Number:3-4
Record Number:CaltechAUTHORS:20161130-111347377
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20161130-111347377
Official Citation:J.S. Levy, J.W. Head, J.L. Dickson, C.I. Fassett, G.A. Morgan, S.C. Schon, Identification of gully debris flow deposits in Protonilus Mensae, Mars: Characterization of a water-bearing, energetic gully-forming process, Earth and Planetary Science Letters, Volume 294, Issues 3–4, 1 June 2010, Pages 368-377, ISSN 0012-821X, http://dx.doi.org/10.1016/j.epsl.2009.08.002. (http://www.sciencedirect.com/science/article/pii/S0012821X09004580)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:72447
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:30 Nov 2016 19:18
Last Modified:09 Mar 2020 13:18

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