We study the dynamics of a stepped crystal surface during evaporation,
using the classical model of Burton, Cabrera and Frank, in which the
dynamics of the surface is represented as a motion of parallel, monato
mic steps. The validity of the continuum approximation treated by Fran
k is checked against numerical calculations and simple, qualitative ar
guments. The continuum approximation is found to suffer from limitatio
ns related, in particular, to the existence of angular points. These l
imitations are often related to the adatom detachment rate which is hi
gher on the lower side of each step than on the upper side ('Schwoebel
effect').