Using inelastic neutron scattering, we have measured a range of amorphous f
orms of ice, including high-density and low-density amorphous ices, in the
energy transfer region from 2 to 500 meV (16-4033 cm(-1)). The measured spe
ctra show that the pressure-produced high-density amorphous ice is signific
antly different from the two low-density amorphous forms of ice (obtained b
y vapor deposition and by annealing at 120 K of the high-density amorphous
ice), as we expected. However, considerable differences were also observed
between the vapor deposits and the low-density amorphous ice obtained from
annealing the high-density amorphous ice (the latter has a spectrum very si
milar to ice-Ih and ice-Ic), indicating that the hydrogen bonding in the tw
o systems are markedly different.