Lunar and Planetary Science XXIX 1866.Pdf
Lunar and Planetary Science XXIX 1866.pdf GALILEO AT CALLISTO: OVERVIEW OF NOMINAL MISSION RESULTS. J. E. Klemaszewski, R. Greeley, K.S. Homan, K.C. Bender, F.C. Chuang, S. Kadel;1 R.J. Sullivan;2 C. Chapman, W.J. Merline;3 J. Moore;4 R. Wagner, T. Denk, G. Neukum;5 J. Head, R. Pappalardo, L. Prockter;6 M. Belton;7 T.V. Johnson;8 C. Pilcher9 and the Galileo SSI Team. 1Dept. of Geology, Arizona State University, Tempe, AZ 871404; 2Cornell Univ., Ithaca, NY; 3SWRI, Boulder, CO; 4NASA Ames, Moffett Field, CA; 5DLR, Berlin, Germany; 6Brown Univ., Providence, RI; 7NOAO, Tucson, AZ; 8JPL, Pasadena, CA; 9NASA HQ, Washington, DC. The solid-state imaging (SSI) system on board the over 4000 and 1600 km in diameter; their Galileo orbiter acquired 118 images of the Jovian morphologies and theories concerning their origin satellite Callisto on 8 of its 11 nominal mission orbits. have been described by many investigators [e.g. On three of these orbits clear-filter imaging data were 2,3,6,8,9]. Whether or not Callisto is differentiated acquired at resolutions of 150 m/pxl or better, and on could not be determined from Voyager data [6]. five orbits color data were acquired at resolutions Galileo mission objectives for Callisto [10] include (a) between 13.7 and 1.1 km/pixel. Galileo images reveal the characterization of surface processes and that degradational processes have acted on the surface materials, (b) impact craters morphologies and of Callisto causing the erosion of crater walls and rims. evolution, (c) the search for evidence of endogenic This degradation is most likely responsible for the activity, (d) the determination of the origin and production of the dark material that appears to blanket morphology of multi-ring structures, and (e) Callisto’s surface, resulting in a lack of small (<10 km comparison of Callisto and Ganymede.
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