Transitional morphology in west Deuteronilus Mensae, Mars - Implications for modification of the lowland/upland boundary

Physics

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Mars Surface, Planetary Structure, Terrain Analysis, Topography, Mars Craters, Mars Photographs, Plains, Planetary Mapping

Scientific paper

The present examination of the west Deuteronilus Mensae region of Mars notes the changes in fretted terrain across the gradational boundary from uplands to lowlands to include a reduction of canyon wall slopes and depths, so that the fretted terrain north of the gradational boundary appears matted, but not obscured. The two process-classes that may account for the lateral overlap are the erosion of stratified upland terrain, and the deposition of plains materials onto the sloping upland margin and fretted terrain. A variety of plains-emplacement mechanisms is considered.

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