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Encyclopedia > Amazonis Planitia

Amazonis Planitia is one of the smoothest plains on Mars. It is located between the Tharsis and Elysium volcanic provinces to the west of Olympus Mons in the Valles Marineris region of the Memnonia quadrangle. Its topography exhibits extremely smooth features at several different lengths of scale. [1] Amongst the findings from the Opportunity rover is the presence of hematite on Mars in the form of small spheres on the Meridiani Planum. ... Categories: Stub | Mars ... Olympus Mons Olympus Mons (Latin, Mount Olympus) is the tallest known mountain in our solar system, located on the planet Mars at approximately 18° N 226° E. In the days before space probes revealed its identity as a mountain, Olympus Mons was known to astronomers as the albedo feature, Nix... Valles Marineris cuts a wide swath across the face of Mars Valles Marineris (Latin for Mariner Valley, named after the Mariner 9 Mars orbiter of 1971-72 which discovered it. ...


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Amazonis Planitia: The role of geologically recent volcanism and sedimentation in the formation of the smoothest ... (537 words)
Amazonis Planitia: The role of geologically recent volcanism and sedimentation in the formation of the smoothest plains on Mars
Amazonis Planitia, located between the two main volcanic provinces on Mars (Tharsis and Elysium), is characterized by extremely smooth topography at several scale lengths, as smooth as oceanic abyssal plains topography on Earth.
Citation: Fuller, E., and J. Head III (2002), Amazonis Planitia: The role of geologically recent volcanism and sedimentation in the formation of the smoothest plains on Mars, J.
MarsDVD.com (1774 words)
The central part, which is dominated by light-colored, relatively smooth to hummocky plains of Amazonis Planitia, is partly bounded to the east by the western flank of the largest known volcano in the solar system, Olympus Mons, and its associated aureole deposits.
Moderately cratered knobby terrain is west of the plains of Amazonis Planitia.
The highlands are separated from the northern plains of Elysium Planitia by a highly dissected, discontinuous northwest trending scarp.
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