The selection of the Discovery Program InSight landing site took over four years from initial
identification of possible areas that met engineering constraints, to downselection via …

Unraveling the stratigraphic record is the key to understanding ancient climate and past
climate changes on Mars (Grotzinger, J. et al.[2011]. Astrobiology 11, 77–87). Stratigraphic …

Abstract Floor-Fractured Craters (FFCs) represent an impact crater type, where the infilling is
separated by cracks into knobs of different sizes and shapes. This work focuses on the …

We present the first Shallow Radar (SHARAD) based observations of subsurface reflections
within an unnamed crater centered at 21.0° S, 150.6° W. It is situated south of the Mangala …

Abstract Endeavour crater (2.28° S, 354.77° E) is a Noachian-aged 22 km-diameter impact
structure of complex morphology in southern Meridiani Planum. The degradation state of the …

Many of the sedimentary basins of Mars show patterns of faults and off-horizontal layers that,
if correctly understood, could serve as a key to basin history. Sediment compaction is a …

The use of numerical datasets of the same type derived from remote sensing instruments is
often treated as equivalent in value and utility, within the limits of their spatial resolution …

We review the methods and data sets used to determine morphometric parameters related
to the depth (eg, rim height and cavity depth) and diameter of Martian craters over the past …

Kilometer-scale pits are nested in the centers of many impact craters on Mars as well as on
icy satellites. They have been inferred to form in the presence of a water–ice rich substrate; …

Abstract Bakhuysen Crater is a Late Noachian to Early Hesperian age∼ 150 km-diameter
impact structure located in the heavily cratered southern highlands of Mars. It is one of the …