Structural glaciology of a glacier confluence, Kaskawulsh glacier, Yukon Territory, Canada

Reports a 1964-65 summer investigation of the north and central arms of this glacier with reference to surface ice deformation at a glacier confluence and its relation to optic-axis fabrics of the ice. The fabrics are concluded to be a result of synkinematic recrystallization, although the nature of the control of this recrystallization is not known.