jbishop-martian-minerals-figure-1-final (IMAGE)
Caption
Figure 1 Mineralogical map of Jezero crater explored by the Perseverance rover. This mineral map was created from near-infrared (1-2.6 µm) CRISM imagery (Parente et al., 2021) using recently developed technologies (Itoh et al., 2021; Saranathan et al., 2021) and overlain on High Resolution Imaging Science Experiment (HiRISE ) imagery. The basaltic rocks at the landing site are dominated by the minerals olivine (red) and pyroxene (tan). Further west, in regions called the Western Fan and Margin Unit, sedimentary rocks predominate. Smectite clay minerals rich in iron and magnesium (light to dark blue tones) and carbonate rich in magnesium and iron (green-yellow tones) were formed through aqueous processes. Unusual iron phosphate and iron sulfide minerals were found at the Bright Angel and Masonic Temple sites near Neretva Vallis (Hurowitz et al., 2025). Other iron phosphate minerals were observed at the Onahu site in the Western Fan region.
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M. Parente
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