The experimentally determined marked rise of the stress intensity factor re
quired to initiate crack propagation in brittle solids under variably high
loading rates, is analyzed. This problem of fracture initiation at the tip
of a crack is considered in terms of activating a flaw at some distance awa
y from the tip. By using a semi-infinite crack in an unbounded two-dimensio
nal solid subjected to spatially uniform but temporally varying crack-face
pressure, we consider the evolution of stress at the failure initiation sit
e. Fracture initiation is assumed synonymous with attaining a critical stre
ss at the fracture site. The results conform to typical experimental data o
f dynamic crack initiation in brittle solids.