Simulations have shown that as two metal surfaces approach each other,
the surface layers can avalanche together when the rigid interfacial
spacing falls below a critical distance. This is accompanied by a disc
ontinuous decrease in the adhesive energy. Here we present an examinat
ion of this phenomenon for the bce metals Fe and W using the Equivalen
t Crystal Theory. In order to identify the circumstances under which a
valanche might be inhibited, the effect of loss of registry between th
e two surfaces is investigated in detail. The avalanche is inhibited w
hen the two surfaces are sufficiently far out of registry and when onl
y a few layers near the surface are allowed to relax. As the relaxing
slabs get thicker a sharp avalanche reappears. However, as the loss of
registry increases the energy released in the avalanche decreases.