ICARUS 120, 119±139 (1996) ARTICLE NO. 0041 Geology of 243 Ida R. SULLIVAN,R.GREELEY, AND R. PAPPALARDO Department of Geology, Box 871404, Arizona State University, Tempe, Arizona 85287-1404 E-mail:
[email protected] E. ASPHAUG,J.M.MOORE, AND D. MORRISON Space Sciences Division, NASA-Ames Research Center, Moffett Field, California 94035-1000 M. J. S. BELTON National Optical Astronomy Observatories, 950 N. Cherry Avenue, Tucson, Arizona 85719 M. CARR Branch of Astrogeologic Studies, MS-946, United States Geological Survey, 345 Middle®eld Road, Menlo Park, California 94025 C. R. CHAPMAN Planetary Science Institute, 620 N. 6th Street, Tucson, Arizona 85705 P. GEISSLER AND R. GREENBERG Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona 85721 JAMES GRANAHAN Hawaii Institute of Geophysics, University of Hawaii at Manoa, 2525 Correa Road, Honolulu, Hawaii 96822 J. W. HEAD III Department of Geological Sciences, Box 1846, Brown University, Providence, Rhode Island 02912 R. KIRK AND A. MCEWEN United States Geological Survey, 2255 N. Gemini Drive, Flagstaff, Arizona 86001 AND P. LEE,P.C.THOMAS, AND J. VEVERKA Center for Radiophysics and Space Research, Cornell University, Ithaca, New York 14853-6801 Received April 3, 1995; revised August 21, 1995 greater than the 1 : 5 ratios common on other rocky bodies. The surface of 243 Ida is dominated by the effects of impacts. Contributing causes include rim degradation by whole-body No complex crater morphologies are observed. A complete ``ringing,'' relatively thin ejecta blankets around crater rims, range of crater degradation states is present, which also reveals or an extended strength gradient in near-surface materials due optical maturation of the surface (darkening and reddening to low gravitational self-packing.