Sediment movement and dispersal patterns on the Grand Banks continental shelf and slope were tied to the dynamics of the Laurentide ice-sheet margin

Harunur Rashid1, Kevin MacKillop2, David Piper3, Marli Vermooten4, Jenna Higgins3, Brittany Marche4, Keesha Langer4, Brent Brockway4, Heather E. Spicer4, Micheala D. Webb4 and Emilie Fournier4, (1)Memorial University of Newfoundland Grenfell, Corner Brook, NF, Canada, (2)Geological Survey of Canada Atlantic, Dartmouth, NS, Canada, (3)Bedford Institute of Oceanography, Dartmouth, NS, Canada, (4)Memorial University of Newfoundland Grenfell, Corner Brook, Canada