2015 GSA Annual Meeting in Baltimore, Maryland, USA (1-4 November 2015)

Paper No. 264-10
Presentation Time: 10:30 AM


ABOTALIB, Abotalib Z., Geosciences, Western Michigan University, 1903 W. Michigan Ave, Kalamazoo, MI 49008; Geology department, National Authority for Remote Sensing and Space Sciences, Cairo, Egypt, SULTAN, Mohamed, Geosciences, Western Michigan University, 1903 W. Michigan Ave, Kalamazoo, MI 49008-5241, ELKADIRI, Racha, Geosciences, Middle Tennessee State University, Murfreesboro, TN 37132, HEGGY, Essam, Jet Propulsion Laboratory, Pasadena, CA 91109; Geosciences, Western Michigan University, 1903 W Michigan Ave, Kalamazoo, MI 49008-5241 and SAAD, Ahmed M., Geology department, Al Azhar University, Cairo, Egypt, abotalibzakia.farag@wmich.edu

The origin of the Martian outflow channels (OC) remains a subject of debate. Two popular models were proposed: groundwater sapping and megaflooding. Understanding the origin of the OC can provide constraints on the presence of life on Mars and on its timing. We adopted an integrated approach (remote sensing, geo-statistical, isotopic, geotechnical and field) to assess the origin of theater-headed valleys (THV) in the Sahara as a potential terrestrial analogue to the Martian landscape. Our findings include: (1) the Saharan THV are widely and densely distributed along fault-controlled escarpments, (2) although extensive erosion was associated with the Saharan THV (typical erosional volume: 2 x 109 m3 to 3 x 109 m3), watershed analysis revealed small upslope contributing areas (typically 8 to 12 km2), (3) escarpments strongly dissected by THV are characterized by strong-over-weak stratigraphy (capping limestone/sandstone: 27 to 52 N/mm2; underlying shale: 14-16 N/mm2) and show evidence of salt weathering (e.g. tafoni, granular disintegration, gypsum veins, polygonal halite crust) and dissolution features (4) spatial analysis reveal a strong spatial correlation between the distribution of THV, tufa and the majority of playas, (5) isotopic composition (δ18O) of tufa deposits (147 samples) are consistent with deposition from depleted fossil Nubian groundwater (δ18O: -12.8 to -8.0 ‰), and (7) geotechnical properties of the Moghra shale in the Qattara depression indicate that shale deposits have high swelling potential. We interpret these findings to indicate that pressurized groundwater accessed deep-seated faults, caused prolonged and extensive discharge, incised THV, facilitated salt weathering, caused basal support swelling, undermined escarpments, caused scarp retreat, deposited tufa on escarpment faces and playa deposits proximal to these cliffs, and modified the Saharan landscape. Because previous research and our analysis of MOLA, HRSC, MARSIS-SHARAD, and THEMIS images indicate that the Martian OC and the Saharan THV and their surroundings share similar morphological characteristics, extensive distribution, high structural control and absence of upslope streams, we suggest that groundwater sapping could have played a major role in the formation of the OC on Mars.