A recently reported occurrence of the Bitterroot, Lewisia rediviva, in southwestern Alberta has been interpreted by its discoverers as a result of modern wind-assisted dispersal across the continental divide. This paper examines evidence that would support an alternative of cultural dispersal by native or non-native groups, and other evidence in support of natural dispersal by range expansion during intervals of xeric conditions in the Holocene. Both hypotheses withstand initial scrutiny, indicating that the wind-dispersal hypothesis should be used with caution. Resolution of the question of dispersal mechanism has broad implications for other species of the southwestern Alberta flora.