THEMIS‐VIS Investigations of Sand at Gale Crater. Issue 8 (11th August 2018)

• Record Type: Journal Article
• Authors: Bennett, Kristen A.; Hill, Jonathon R.; Murray, Kimberly C.; Edwards, Christopher S.; Bell, James F.; Christensen, Phillip R.
• Is Part Of: Earth and space science. Volume 5:Issue 8(2018)
• Page Start: 352
• Page End: 363
• Publication Date: 2018-08-11
• Subjects: Mars -- sand -- Gale crater -- color mosaic; Space sciences -- Periodicals; Geophysics -- Periodicals; 500.5
• DOI: 10.1029/2018EA000380
• Languages: English
• ISSNs: 2333-5084

Abstract

Abstract: Gale crater is the landing site of the Mars Science Laboratory (MSL) rover, Curiosity. Here we present Thermal Emission Imaging System Visible Imaging Subsystem (THEMIS‐VIS) mosaics in gray scale and in false color of Gale crater. We use these data products, in addition to THEMIS thermal infrared decorrelation stretch (DCS) mosaics, thermal inertia derivations, and near‐infrared spectra to investigate the MSL traverse area and sand across Gale crater. We identified several THEMIS‐VIS color units in the MSL traverse area that may correlate to the amount of sand cover that is present on each unit. This suggests that THEMIS‐VIS color is extremely useful in identifying dark basaltic sand, which appears as blue in THEMIS‐VIS false color images. We test this hypothesis by identifying small (~several pixels) blue patches on the southeast side of the central mound in Gale crater and confirming that they are patches of sand in High Resolution Imaging Science Experiment (HiRISE) images. Sand dunes on the crater floor exhibit variations in all data sets utilized in this study, with the Bagnold dunes and the western sand sea exhibiting the most notable differences. We propose that these differences are the result of a thin layer of dust that covers the western sand sea, although we do not rule out possible effects from grain size sorting. Key Points: THEMIS‐VIS color and gray scale mosaics of Gale crater were created and used to investigate color variability in the MSL traverse region THEMIS‐VIS false color images can be used to identify small (tens of meters) patches of dark toned sand on the Martian surface Differences between the Bagnold dunes and the western sand sea are likely due to a thin layer of dust on the sand sea