The coquina clam, Donax variabilis, rides flow from waves, migrating s
horeward during rising tides and seaward during falling tides. This me
thod of locomotion, swash-riding, is controlled not only behaviorally
but also morphologically. The shape of this clam causes it to orient p
assively; a clam rotates in flow, usually in backwash, until its anter
ior end is upstream. Rotation is about a vertical axis through a pivot
al point where the shell touches the sand. The density, weight distrib
ution, and wedge-like shape are all important in effecting orientation
. Such orientation is significant because it contributes to stability
of motion. On an unoriented clam, upward lift can be higher than its u
nderwater weight-a circumstance that results in uncontrollable tumblin
g. In contrast, once oriented with its anterior end upstream, a clam e
xperiences downward lift that contributes to its stability while slidi
ng in backwash. Furthermore, when the anterior end is upstream, drag i
s reduced relative to when the ventral, dorsal, or posterior ends are
upstream. Since orientation occurs only above a minimum velocity, it h
as the effect of slowing a clam's motion over the substratum in rapid
flows. Stability, drag, and speed reduction enhance a clam's ability t
o gain a foothold and dig in after a swash-ride, before wave flows can
wash it off the beach and out to sea.