The Medusae Fossae formation, Amazonis Planitia, Mars - Evaluation of proposed hypotheses of origin

Mathematics – Logic

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Mars Surface, Mineral Deposits, Viking Spacecraft, Planetary Geology, Lava, Planetary Evolution, Highlands, Terrain Analysis, Image Resolution, Carbonates, Satellite Imagery

Scientific paper

Thick (up to 3 km) and areally extensive (over 2 million sq km) deposits in the Amazonis Planitia region of Mars cover both the heavily cratered highland terrain south of the equator and moderate- to lightly-cratered plains north of the highlands. These enigmatic materials have been mapped as the Medusae Fossae Formation (MFF). We have begun a reexamination of the MFF deposits in an attempt to establish constraints that may help to discriminate between the various working hypotheses of origin. Excellent Survey mission Viking images show a wealth of morphologic detail exposed within the MFF deposits. Through a combination of geologic mapping, remote sensing data analysis, and consideration of likely terrestrial analogs, a list of the most viable hypotheses may be produced and certain key future observations identified to refine the proposed hypotheses.

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