The observed minimum in the normal stress beneath the highest portion
of a 'sandpile' (a pile of granular material) is a counter-intuitive r
esult that has long remained unexplained. In this paper, we suggest th
at spatial size differentiation, where the larger particles are separa
ted from smaller particles within the pile, creates an increase in the
internal horizontal stress distribution, which in turn gives rise to
a minimum in the normal stress, similar to what is observed experiment
ally. We develop a simple analytic model for the normal stress that en
capsulates the existence of horizontal contact forces between adjacent
colevel particles. We compare this analytic model to the results of a
n n-body simulation code, where we obtain close quantitative agreement
for small sandpiles. Finally, experimental results from a real sandpi
le are replicated by an n-body code, but only for a distribution of ma
terial where the largest particles are at the top of the pile.