An absorption band at 260 nanometers on the trailing hemisphere of Gan
ymede, identified as the Hartley band of ozone (O-3), was measured wit
h the Hubble Space Telescope, The column abundance of ozone, 4.5 x 10(
16) per square centimeter, can be produced by ion impacts or by photoc
hemical equilibrium with previously detected molecular oxygen (O-2). A
n estimated number density ratio of [O-3]/[O-2] approximate to 10(-4)
to 10(-3) requires an atmospheric density orders of magnitude higher t
han upper limits from spacecraft occultation experiment's. Apparently,
this O-2-O-3 ''atmosphere'' is trapped in Ganymede's surface ice, an
inference consistent with the shift and broadening of the band compare
d with the gas-phase O-3 band.