When a mixture of small and large grains is poured between two vertica
l slabs, the mixture spontaneously stratifies in alternating layers of
small and large grains. We describe a possible mechanism and we devel
op a model that reproduces stratification of the large and small grain
s in alternating layers. We find that the requirement for stratificati
on is that the angle of repose of the large pure species is larger tha
n the angle of response of the small pure species, prediction confirme
d by the experimental findings. (C) 1998 Elsevier Science B.V. All rig
hts reserved.