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Here we use gravity and topography analyses to show that the crustal dichotomy boundary was excavated by only one later impact basin (Isidis), which probabilistiy indicates that fewer than 12 large basins across the globe could post-date the boundary and pre-date the established younger basins.
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Moreover, the relatively pristine topography and crustal thickness at the dichotomy boundary indicates that younger basins should be similarly well preserved.
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Cosmogenic nuclide surface exposure ages have been widely used to constrain glacial chronologies in the European regions.
Determining the age of surfaces on Mars
This paper brings new evidence that the Romanian Carpathians sheltered mountain glaciers in their upper valleys and cirques until the end of the last glaciation.
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