Little is known about the internal properties of Callisto-the outermos
t of Jupiter's four large galilean moons-other than the average densit
y (about 1.8 cm(-3)). The recent unexpected discovery(1-4) that Ganyme
de, and perhaps Io, has an internally generated magnetic field, combin
ed with gravity results(5,6) suggesting that both Ganymede and Io are
internally differentiated with metallic cores and rocky mantles, has h
eightened anticipation of the results obtained by the Galileo spacecra
ft in its recent fly-by of Callisto. Here we report that the spacecraf
t, passing the moon at a distance of only similar to 1,100 km from the
surface, detected only a small enhancement of the field strength (sim
ilar to 7 nT), which may be related to changes in the jovian plasma en
vironment caused by Callisto(7). Callisto does not have an internally
generated magnetic field.