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Cette carte conceptuelle, cree avec IHMC CmapTools, contient des informations liees a : Gusev Crater, Gusev Crater: Candidate Landing Site is located at 0 km elevation, Aqueous Sediment are composed of Materials from Multiple Ages & Geologic Units, Favorable Landing Condition is helped by Low Basin Topography, 14.5S/184.5W lies within Highlands, Thyra Crater is 20 km in Diameter, Aqueous Sediment are partially exposed in Thyra Crater, Hesperian Era to Amazonian Era Lake Episodes deposited Aqueous Sediment, Delta of Gusev Crater is 300 to 500 m High, Favorable Landing Condition is helped by Earth-based Radar Data, Aqueous Sediment by freezing may have favored the generation of Ice-Cored Mounds/ Pingos, 170-km Crater Basin with Low Basin Topography, Delta of Gusev Crater exposes Materials from Multiple Ages & Geologic Units, Water was supplied by Ma'adim Vallis, Favorable Landing Condition is helped by Thermal Inertia sup.4, Ma'adim Vallis formed an Intravalley Lake, Gusev Crater: Candidate Landing Site was formed in the Highlands, Ma'adim Vallis created the Delta of Gusev Crater, Water and Climate, Evidence of Past Life may be associated with Hydrothermal Systems, Gusev Crater: Candidate Landing Site was generated from a Giant Impact