When grains are added to a large sandpile, quasiperiodic large avalanc
hes maintain the steady state mass. The buildup periods between the la
rge avalanches contain many small avalanches. The size distribution of
the small events does not vary during a buildup period but their mean
rate of occurrence does. The qualitative behavior of the real sandpil
e avalanches is identical to the behavior of earthquakes on a model fa
ult proposed by Carlson and Langer. As that model suggests, the runnin
g total number of small avalanches can in principle predict the occurr
ence of the large avalanches.