  We consider the growth of a vicinal crystal surface in the presence of a
step-edge barrier. For any value of the barrier strength, measured by the
length l_es, nucleation of islands on terraces is always able to destroy
asymptotically step-flow growth. The breakdown of the metastable step-flow
occurs through the formation of a mound of critical width proportional to
L_c=1/sqrt(l_es), the length associated to the linear instability of a
high-symmetry surface. The time required for the destabilization grows
exponentially with L_c. Thermal detachment from steps or islands, or a steeper
slope increase the instability time but do not modify the above picture, nor
change L_c significantly. Standard continuum theories cannot be used to
evaluate the activation energy of the critical mound and the instability time.
The dynamics of a mound can be described as a one dimensional random walk for
its height k: attaining the critical height (i.e. the critical size) means that
the probability to grow (k->k+1) becomes larger than the probability for the
mound to shrink (k->k-1). Thermal detachment induces correlations in the random
walk, otherwise absent.
