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1 tosphere) in the vicinity of both Europa and Callisto.
2 nificantly younger than that of Ganymede and Callisto.
4 evidence for internal liquid water oceans in Callisto and Europa, detection of a strong intrinsic mag
5 surface materials of the Galilean satellites Callisto and Ganymede from analysis of reflectance spect
7 e and a tenuous carbon dioxide atmosphere at Callisto, and detection of condensed oxygen on Ganymede.
10 ect information on the interior structure of Callisto determined from previous spacecraft fly-bys was
11 meter have indicated that neither Europa nor Callisto have an appreciable internal magnetic field, in
12 (C10) indicate that the rock and ice within Callisto have partially, but not completely, separated.
16 alilean satellites--Io, Europa, Ganymede and Callisto-ranged from uniform mixtures of rock and ice (t
18 to a rock-metal core less than 25 percent of Callisto's radius, an outer layer of clean ice less than
21 hs of impact craters on Europa, Ganymede and Callisto that reveal two anomalous transitions in crater
22 ncounter (C3) of the Galileo spacecraft with Callisto, the outermost Galilean moon of Jupiter, indica
25 s to the galilean moons Europa, Ganymede and Callisto, which reside within Jupiter's radiation belts.
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