Original metadata (https://open.yukon.ca) (English, HTML)
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- 2026-09-09
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.
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