Instead of the expected erosion morphology composed of craters, rare gas io
n bombardment of the, Al(111) surface is found to cause initial surface gro
wth of several atomic layers. This phenomenon is observed for Ne+, Ar+. and
Xe+ at all temperatures at which bombardment induces morphological surface
changes and for ion energies down to a few hundred eV. Thr effect is inter
preted on the basis of a thermal spike induced separation of damage into su
bsurface vacancy clusters and surface allatum clusters.