Ice stream retreat dynamics inferred from an assemblage of landforms in the northern Barents Sea

Two directions of past ice flow are indicated from streamlined glacial landforms in the study area. Ice flow from north north-east is indicated for the Last Glacial Maximum and an early phase of deglaciation, whereas a shift to flow from north north-west, from an ice dome located over Hinlopenstretet, Svalbard is indicated for the latest deglaciation phases of the Bjørnøyrenna Ice Stream.