The structure of the regolith on 67P/Churyumov-Gerasimenko from ROLIS descent imaging

The structure of the upper layer of a comet is a product of its surface activity. The Rosetta Lander Imaging System (ROLIS) on board Philae acquired close-range images of the Agilkia site during its descent onto comet 67P/Churyumov-Gerasimenko. These images reveal a photometrically uniform surface c...

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Veröffentlicht in:Science (American Association for the Advancement of Science) 2015-07, Vol.349 (6247), p.495-495
Hauptverfasser: Mottola, S., Arnold, G., Grothues, H.-G., Jaumann, R., Michaelis, H., Neukum, G., Bibring, J.-P., Schröder, S. E., Hamm, M., Otto, K. A., Pelivan, I., Proffe, G., Scholten, F., Tirsch, D., Kreslavsky, M., Remetean, E., Souvannavong, F., Dolives, B.
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Sprache:eng
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Zusammenfassung:The structure of the upper layer of a comet is a product of its surface activity. The Rosetta Lander Imaging System (ROLIS) on board Philae acquired close-range images of the Agilkia site during its descent onto comet 67P/Churyumov-Gerasimenko. These images reveal a photometrically uniform surface covered by regolith composed of debris and blocks ranging in size from centimeters to 5 meters. At the highest resolution of 1 centimeter per pixel, the surface appears granular, with no apparent deposits of unresolved sand-sized particles. The thickness of the regolith varies across the imaged field from 0 to 1 to 2 meters. The presence of aeolian-like features resembling wind tails hints at regolith mobilization and erosion processes. Modeling suggests that abrasion driven by airfall-induced particle "splashing" is responsible for the observed formations.
ISSN:0036-8075
1095-9203
DOI:10.1126/science.aab0232