| Moons The four large Galilean
Satellites of Jupiter (from left to right
in mosaic: Io, Europa, Ganymede, and
Callisto) resemble a miniature solar
system. The global density, relative
amount of rocky material, and duration
and intensity of geologic activity on
each satellite all decrease with
increasing distance from Jupiter. Each
satellite is very distinctive in
appearance and geologic history. Io, the
densest and innermost major satellite, is
volcanically active today. Europa has a
highly fractured, young icy outer shell.
Ganymede has a complex volcanic and
tectonic history, and Callisto, the least
dense and outermost satellite, is heavily
cratered and rather bland by comparison.
The geologic histories of these
satellites are related to tidal
deformation and heating, which is more
intense closer to Jupiter.
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