Abstract
Humlum. Ole: Altitudinal trends of talus-derived lobate rock glaciers on Disko, central West Greenland. Geografisk Tidsskrift 84: 35–39, Copenhagen. January 1984. Talus-derived lobate (TDL) rock glaciers follow the altitudinal trend of the equilibrium line (ELA) on contemporary glaciers, and based on an analysis of a cross-section, North Disko, it is suggested that the vertical distance between the zone of TDL-rock glaciers and the lowermost occurrence of tongue-shaped rock glaciers relate to the amount of precipitation.
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