The potential for collapse due to a reduction in confinement is evalua
ted for two very different soils: a uniformly graded sand and an undis
turbed clayey colluvial soil. Soil specimens were consolidated anisotr
opically and subjected to constant-shear-drained (CSD) tests. During t
he CSD lest, the effective confining pressure is gradually reduced whi
le the shear stress is held constant. Only for very loose specimens is
collapse observed before the failure envelope or steady state is reac
hed. In general, specimens subjected to the CSD stress path behave dif
ferently than specimens of similar initial density and confining press
ure subjected to typical compression stress paths. This observation in
dicates that knowledge of the stress path is necessary to accurately p
redict the collapse potential, and thereby the potential for flow fail
ure, of loose saturated soils.