45th Lunar and Planetary Science Conference (2014) sess810.pdf
[810] PRINT ONLY: MARS GEOMORPHOLOGY
Arfstrom J. D. A Possible Tunnel Valley Network in East Kasei Valles, Mars [#1013] In east Kasei Valles there is a streamlined hill that appears to be incised by a network of tunnel valleys, suggesting that Kasei Valles is glacial in origin.
Aureli K. L. Goudge T. A. Head J. W. Fassett C. I. Classification of Candidate Impact Crater-Hosted Closed-Basin Lakes on Mars [#2369] We have identified 297 candidate closed-basin lakes within impact craters on Mars with three distinct inlet channel morphologies: long, short, and interior channels.
Biró T. Tectonically Preformed Valley Pattern and Formation Related to Volcanic Structure on Ceraunius Tholus [#1403] A possible tectonic explanation proposed on the specific sinuous structure and on the assimetrical valley pattern on the martian Ceraunius Tholus volcano.
Carr M. H. Head J. W. III Martian Unbound Water Inventories: Changes with Time [#1427] We examine the known water inventory on Mars by dividing it into six reservoirs and documenting their abundances with time.
Coleman N. M. Significance of Crater Lakes on Mars that were Filled and Overtopped by Groundwater [#1293] Martian crater lakes that were filled and overtopped by groundwater (e.g., Morella Crater) provide key data on former pressures in the subcryosphere aquifer.
Crosta G. B. De Blasio F. V. Setting the Stage for a Model of Thermokarst Evolution of Valles Marineris, Mars [#2050] Origin of aligned subcircular subsidence depressions by deep ice sublimation is discussed, suggesting possible future modeling scenarios.
De Blasio F. Investigating the Hydrology of the Alleged Hellas Planitia Lake in Southern Mars [#1511] Some of the possible consequences of water filling the Hellas Planitia impact basin are put forward.
de Pablo M. A. Orosei R. Centeno J. D. Looking for Buried Ice Relict of Glacial Activity at the Lower NW Flank of the Hecates Tholus Volcano on Mars by SHARAD Data [#1151] We use analize SHARAD data to deduce the possible existence of remnant ice lenses under the surface at a place characterized by glacial features on Mars.
Frattini P. Crosta G. B. De Blasio F. V. Castellanza R. Utili S. et al. Crater Shock Damage Zone and Landslide Size Distribution in Valles Marineris, Mars [#2024] Distribution of impact damage zones can control landslide size distribution and location along Valles Marineris. 3-D slope stability analyses are presented.
Giuppi S. Selection of Mars Areas to be Properly Investigated Using MARSIS Radar Data [#1016] In Mars subsurface analysis, radar data quality are effected by surface characteristics, which may introduce undesired clutter effects.
45th Lunar and Planetary Science Conference (2014) sess810.pdf
Hamilton V. E. Vasavada A. R. Christensen P. R. Coordinated MSL and Mars Odyssey Observations of Ground Temperature in Gale Crater, Mars [#1569] The correlation between MSL and ODY ground temperature measurements is very good. In situ data provide insight into the local scale variability in geology.
Hobbs S. W. Paull D. J. Clarke J. D. A. A Hydrological Analysis of Terrestrial and Martian Gullies: Implications for Liquid Water on Mars [#1119] We used Manning and Darcy-Weisbach equations to infer fluid velocities and discharge rates on martian and analogous terrestrial gullies.
Nussbaumer J. W. Evidence for Impact into Ice Rich Terrain and Melting to Produce Glaciation and Valley Networks in the Aeolis/Zephyria Plana Region, Mars [#1122] Valley networks originated from the release of water due to the deposition of hot ejecta over ice deposits present in the area during the impact event.
Rodriguez J. A. P. Gulick V. Baker V. Platz T. Fairén A. G. Evidence for Multiple Stages of Extensive Low Outflow Channel Floor Resurfacing in Southern Circum-Chryse, Mars [#2917] The lower outflow channels of southern circum-Chryse contain extensive chaotic terrains. We propose these were produced by the collapse of ice-rich debris flows.
Sinha R. K. Vijayan S. Murty S. V. S. Modes of Gully Formation Around North East of Argyre Basin and the Role of Volatile Discharge due to Microclimatic Shifts [#1670] Morphological analysis of five different modes of gully formation suggests three distinct phases in which gullies formed around northeast Argyre basin on Mars.
Valbuzzi E. Crosta G.-B. De Blasio F.-V. Probable Rock Falls in the Pits of Arsia Mons, Mars [#2093] HiRISE images show the presence of boulders at the bottom of one pit of Arsia Mons, likely fallen from the flanks similar to rock falls on Earth.
Vijayan S. Sinha R. K. Murty S. V. S. Characteristics of Craters with Multi Layered Ejecta in the Equatorial Region of Mars [#1676] Characteristics of craters with multilayered ejecta based on their inner floor morphology and correlating to their ejecta distribution pattern.