The onset of surface melting at {00.1} (''basal''), {10.0} and {11.0}
(''nonbasal'') surfaces of hexagonal ice is studied experimentally by
glancing-angle X-ray scattering. The preparation of mirror-like single
crystal ice surfaces and a special in situ X-ray chamber is described
in detail. The X-ray scattering experiments using synchrotron radiati
on give clear evidence that all the investigated high-symmetry surface
s exhibit surface melting with onset temperatures T-s congruent to -13
.5 degrees C for the basal and T-s congruent to -12.5 degrees C for th
e nonbasal surfaces. The temperature dependence of the thickness of th
e quasiliquid is presented and discussed in view of various theoretica
l predictions. In addition we found thermal faceting at nonbasal surfa
ces as well as a diffuse (''rough'') solid-quasiliquid interface. The
thermal properties of the observed surface disorder implies that the c
orrelation length within the socalled ''surface melt'' is much larger
than the correlation length in the bulk liquid indicating the presence
of significant ''substrate'' interactions.