Abstract
The prominent Ungava Bay landform swarm (UBLS), covering an area of ˜260000 km2 south of Ungava Bay, Canada, is defined by drumlins, crag‐and‐tails, horned crag‐and‐tails and flutes indicating convergent ice flow towards Ungava Bay. The UBLS has been difficult to interpret in terms of ice‐sheet configuration, dynamics and age. Aerial photograph and satellite image interpretations of the Labrador‐Ungava region reveal a previously unrecognized level of complexity within the UBLS consisting of several well‐defined segments, most interpreted as representing discrete stream‐flow events. Each of the segments is characterized by one or more of the criteria (convergent flow patterns at their heads, attenuated till lineations and abrupt lateral margins) previously suggested as diagnostic for formation by fast‐flowing ice (ice streams). The UBLS reflects the most direct and probably fastest contact (in terms of sediment transport) between the Laurentide Ice Sheet interior and the ocean. It is therefore a prime candidate for abrupt changes in glacial‐age northwest Atlantic seafloor sedimentation.
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