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 Piper2, Marli Vermooten3, Jenna Higgins2, Brittany Marche3, Keesha Langer3, Brent Brockway3, Heather E. Spicer3, Micheala D. Webb3 and Emilie Fournier3, (1)Memorial University of Newfoundland Grenfell, Corner Brook, NF, Canada, (2)Bedford Institute of Oceanography, Dartmouth, NS, Canada, (3)Memorial University of Newfoundland Grenfell, Corner Brook, Canada