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Figure 1. (a) Location of Cross crater on a MOLA topographic map
of Mars where red colors are high elevations and blue are low elevations.
Elevation range is approximately –2500 to 10 000 m. (b) MOLA
topographic map of Cross crater overlain on CTX. (c) Nighttime thermal
infrared map from THEMIS (Christiansen et al. 2004). Bright-toned areas are
warmer and higher thermal inertia. Peak ring materials and bright
sedimentary layers are relatively lower thermal inertia relative to a later
emplaced dark cap rock. (d) CRISM multispectral maps showing the
locations of secondary minerals withinand around Cross crater using
band depth parameterizations (Pelkey et al. 2007). Red = BD1900 for H2O
in mineral structures, green = BD2200 for Al-OH and Si-OH, blue = BD2300
for Fe-OH and Mg-OH. http://dx.doi.org/10.2138/am-2016-5574">