We calculated the stress field on and around an elliptical open crack locat
ed in an elastic medium under various confining pressures. The problems wer
e treated as two-dimensional ones by using complex potentials, and the cons
iderable differences between uniaxial and triaxial crack growth mechanisms
were recognized. A uniaxial condition allows a certain elliptical open crac
k to develop by itself (without any crack-crack interactions) along its maj
or semi-axis, whereas a triaxial condition does not. This is the principal
mechanism of transition from uniaxial to triaxial crack growth. Our transit
ion model, derived using a theoretical approach, explains the dependence of
experimental results, such as crack distribution and internal friction ang
le, on confining pressure well. We conclude that uniaxial and triaxial crac
k growth mechanisms fundamentally differ from each other, and that attentio
n must be paid to experimental conditions when applying experimental result
s to phenomena in the Earth.