The Galileo Orbiter examined several impact features on Europa at cons
iderably better resolution than was possible from Voyager. The new dat
a allow us to describe the morphology and infer the geology of the lar
gest impact features on Europa, which are probes into the crust, We ob
serve two basic types of large impact features: (1) ''classic'' impact
craters that grossly resemble well-preserved lunar craters of similar
size but are more topographically subdued (e.g., Pwyll) and (2) very
flat circular features that lack the basic topographic structures of i
mpact craters such as raised rims, a central depression, or central pe
aks, and which largely owe their identification as impact features to
the field of secondary craters radially sprayed about them (e.g., Call
anish), Our interpretation is that the classic craters (all <30 km dia
meter) formed entirely within a solid target at least 5 to 10 km thick
that exhibited brittle behavior an time scales of the impact events.
Some of the classic craters have a more subdued topography than fresh
craters of similar size on other icy bodies such as Ganymede and Calli
sto, probably due to the enhanced viscous relaxation produced by a ste
eper thermal gradient on Europa, Pedestal ejecta facies on Europa (and
Ganymede) may be produced by the relief-flattening movement of plasti
cally deforming but otherwise solid ice that was warm at the time of e
mplacement, Callanish and Tyre do not appear to be larger and even mor
e viscously relaxed versions of the classic craters; rather they displ
ay totally different morphologies such as distinctive textures and a s
eries of large concentric structural rings cutting impact-feature-rela
ted materials. Impact simulations suggest that the distinctive morphol
ogies would not be produced by impact into a solid ice target, but may
be explained by impact into an ice layer similar to 10 to 15 km thick
overlying a low-viscosity material such as water. The very wide (near
antipodal) separation of Callanish and Tyre imply that similar to 10-
15 km may have been the global average thickness of the rigid crust of
Europa when these impacts occurred. The absence of detectable craters
superposed on the interior deposits of Callanish suggests that it is
geologically young (<10(8) years). Hence, it seems likely that our pre
liminary conclusions about the subsurface structure of Europa apply to
the current day. (C) 1998 Academic Press.