title: Dimensional Fabric and Ice Flow, Precambrian (Huronian) Glaciation.
abstract: The Huronian Cobalt tillite (Gowganda formation) exhibits a preferred dimensional orientation of embedded elongate rock fragments. The orientation is believed to be due to ice motion. Data from four localities show an alignment in about a north-south direction. Data are inadequate to locate center of ice dispersal.
authors.forename: F J
authors.initials: FJ
authors.lastname: Pettijohn