We have studied the effect of nonhydrostatic stresses on the equilibri
um shape of pure helium-4 crystals[1]. First, by applying small stress
es, a macroscopic melting of the crystal is produced which is quadrati
c in the strain and can be quantitatively understood using simple ther
modynamics and elasticity theory[2]. Secondly above a certain threshol
d in strain, easily visible grooves appear on the crystal surface[1][3
]. This is the first quantitative evidence for the general instability
which was first predicted by Grinfeld[4].