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The topography and morphology of low shields and associated landforms of plains volcanism in the Tharsis region of Mars
DOI: 10.1016/j.jvolgeores.2009.04.015 Bibcode: 2009JVGR..185...69H

Hauber, Ernst; Gwinner, Klaus; Greeley, R. +2 more

The morphology and topography of volcanic landforms provide critical information to the investigation of their tectonic setting and the physical characteristics (e.g., rheology) of their eruption products. Their investigation is also an important prerequisite for studies of comparative planetology, (e.g., the comparison between surface features of…

2009 Journal of Volcanology and Geothermal Research
MEx 88
Spatial and alignment analyses for a field of small volcanic vents south of Pavonis Mons and implications for the Tharsis province, Mars
DOI: 10.1016/j.jvolgeores.2009.04.008 Bibcode: 2009JVGR..185...96B

Greeley, Ronald; Williams, David A.; Glotch, Timothy D. +5 more

A field of small volcanic vents south of Pavonis Mons was mapped with each vent assigned a two-dimensional data point. Nearest neighbor and two-point azimuth analyses were applied to the resulting location data. Nearest neighbor results show that vents within this field are spatially random in a Poisson sense, suggesting that the vents formed inde…

2009 Journal of Volcanology and Geothermal Research
MEx 58
Shape, rheology and emplacement times of small martian shield volcanoes
DOI: 10.1016/j.jvolgeores.2009.05.003 Bibcode: 2009JVGR..185...47B

Mangold, N.; Pinet, P.; Baratoux, D. +3 more

This paper focuses on the shape of 31 shield volcanoes of small to intermediate size (a few tens of kilometers in diameter) in 5 regions of Mars: Tempe Terra, Syria Planum, Pavonis Mons, Arsia Mons and central Elysium Planitia. A model for the shape of these shield volcanoes is applied, based upon the concept of porous flow of an unconfined aquife…

2009 Journal of Volcanology and Geothermal Research
MEx 29