The existence of a torus of plasma generated by sputtering from Jupite
r's satellite Europa has long been suspected but never yet convincingl
y demonstrated. Temperature profiles from Voyager plasma observations
indicate the presence of hot, possibly freshly picked-up ions in the g
eneral vicinity of the orbit of Europa, which may be interpreted as ev
idence for a local plasma torus. Studies of ion partitioning in the ou
ter regions of the Io torus reveal that the oxygen to sulfur mixing ra
tio varies with radial distance; this may indicate that oxygen-rich ma
tter is injected from a non-Io source, most probably Europa. We have c
onstructed a quantitative model of a plasma torus near the orbit of Eu
ropa which takes into account plasma input from the Io torus, sputteri
ng from the surface of Europa, a great number of ionization and charge
exchange processes, and plasma loss by diffusive transport. When the
transport time is chosen so that the model's total number density in c
onsistent with the observed total plasma density, the contribution fro
m Europa is found to be significant although not dominant. The model p
redicts in detail the ion composition, charge states, and the relative
fractions of hot Europa-generated and (presumed) cold Io-generated io
ns. The results are generally consistent with observations from Voyage
r and can in principle (subject to limitations of data coverage) be co
nfirmed in more detail by Ulysses.