lpetrich
Contributor
The remaining Galilean moons are Ganymede and Callisto, and both of them have lots of impact craters. Ganymede also has thick light-colored splotches on its surface, though Callisto doesn't.
The two moons have mean densities consistent with much of them being water, whether ice or liquid water. The lower parts of this water may be high-pressure ice and/or mixed with rock. Like Europa, Ganymede and Callisto may also have subsurface oceans. But they don't have nearly at much tidal heating as Io or Europa, at least at present.