title: Knoll and Sediment Drift near Hudson Canyon.
abstract: A parallel-bedded accumulation of sediments forms a low ridge on the upcurrent side of a partially moated knoll. These sediments were deposited beneath a southwestward-flowing current where it is locally decelerated by the obstructing knoll.
authors.forename: A
authors.initials: A
authors.lastname: Lowrie
authors.forename: B C
authors.initials: BC
authors.lastname: Heezen