Experiments on plate-like specimens have established that across-colum
n cracks form within S2 (columnar) salt-water ice when compressed unia
xially along a direction inclined to the long axis of the grains. Wing
cracks initiate from the across-column cracks and lengthen into axial
splits when the ice is rapidly deformed; correspondingly, the macrosc
opic behavior changes from ductile to brittle. The across-column crack
ing is attributed to grain-boundary sliding, and the splitting to the
suppression of crack-tip creep.