In this paper we investigate the stability of interfacial gravity wave
s in an aluminium reduction cell. Specifically, we use an energy argum
ent to unravel the physical mechanisms leading to instability, and to
evaluate wave growth rates. In common with other studies, we find that
the vertical component of the background magnetic field is central to
the instability. Here we show that a key instability mechanism is the
generation of oscillatory motion in a direction parallel to the wave
crests. This induced, transverse motion is in-phase with the wave pres
sure, and so transfers energy into the disturbance.