In a first-order wetting transition it is possible to overheat a micro
scopic layer from below to above the wetting temperature T(w), and to
undercool a macroscopic layer from above to below T(w). in both cases
the transition to stable equilibrium occurs by formation and growth of
supercritical nuclei. The critical nuclei for overheating are droplet
s on the wall of the system and for undercooling they are dents in the
macroscopic layer. A recent calculation of the critical droplet in a
special dimension d0 is now supplemented by the calculation of the cri
tical dent for dewetting. Although the analytic expressions for the pr
ofiles are closely related, the nuclei above T(w) are finite whereas t
hey are infinitely large below T(w). The latter is to be expected sinc
e the system is infinitesimally close to coexistence of wet and non-we
t states at all temperatures T< T(w).