Using He atom scattering, layer-by-layer erosion of InSb(110) by low e
nergy ion bombardment has been observed to proceed via nucleation of v
acancy islands, island growth and coalescence. The mechanism is in ful
l agreement with theoretical models developed for crystal growth, with
diffusing adatoms substituted by diffusing vacancies. In particular i
t has been observed that coalescence of the vacancy islands sets in af
ter the removal of small fractions of a monolayer and that the average
terrace width increases with number of sputtered monolayers.