We show that tilting a model sandpile that has dynamic disorder leads to bi
stability and hysteresis at the angle of repose. Also the distribution of l
ocal slopes shows an interesting dependence on the amount of tilt weakly ti
lted sandpiles retain the quasicontinuous distributions of the steady state
while large tilt makes the distribution more discrete with local slopes cl
ustered round particular values. These observations are compared with recen
t experimental results on avalanche shapes. We also consider the percolatio
n of local instability and anomalous roughening of the sandpile surface.