Under across-column uniaxial and biaxial compression loading of column
ar ice polycrystals in the brittle regime, a set of cracks that split
the columnar grains has been observed. However, both the mechanism res
ponsible for their nucleation and a quantitative description of the st
ress associated with such events have remained unresolved in the liter
ature. In this paper, we first show that the nucleation of such cracks
is consistent with the sliding of grain Facets along the column axes,
and then describe a fracture mechanics-based model that correctly pre
dicts their nucleation stress. (C) 1977 Acta Metallurgica Inc.