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Submarine Mass Movements and Their Consequences
In Hudson Bay and Hudson Strait, the rapid collapse of the Laurentide Ice Sheet (LIS) culminated in the catastrophic drainage of proglacial Lake Agassiz into the North Atlantic around 8500 cal BP. It has been suggested that this catastrophic event may have triggered the 8200 cal BP cold event recorded in Greenland ice cores. Evidence for that outburst flood was the identification of a centimeter to decimeter-thick hematiterich red layer that was observed in Hudson Strait sediments around 8000doi:10.1007/978-1-4020-6512-5_14 fatcat:gn76znicufbuxdo4sp3c22xbpm