Let's restrict ourselves to deep ocean waves, where the ``restoring force'' is simply gravity. (When a wave reaches shallow water, the bottom provides an immobile boundary that complicates matters severely, as anyone knows who has ever watched surf breaking on a beach!) The motion of an ``element'' of water in such a wave is not simply ``up and down'' as we pretended at the beginning of this chapter, but a superposition of ``up and down'' with ``back and forth'' in the direction of wave propagation. A cork floating on the surface of such a wave executes circular motion, or so I am told. (It is actually quite difficult to confirm this assertion experimentally since it requires a fixed reference that is not moving with the water - a hard thing to arrange in practice without disturbing the wave itself.) More importantly, the propagation velocity of such waves is higher for longer wavelength.