Dimensional Fabric and Ice Flow, Precambrian (Huronian) Glaciation

Science  09 Feb 1962:
Vol. 135, Issue 3502, pp. 442
DOI: 10.1126/science.135.3502.442


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.