A widely applicable analysis of numerical data shows that, while the distri
bution of avalanche areas obeys finite size scaling, that of toppling numbe
rs is universally characterized by a full, nonlinear multifractal spectrum.
Boundary effects determine an unusual dependence on system size of the mom
ent scaling exponents of the conditional toppling distribution at a given a
rea. This distribution is also multifractal in the bulk regime. The resulti
ng picture brings to light unsuspected physics of this long-studied prototy
pe model.