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December 16, 1966

Sediment transport in a Precambrian ice age: The Huronian Gowganda Formation Sediment transport in a Precambrian ice age: The Huronian Gowganda Formation

The Gowganda Formation of Ontario consists of conglomerates, quartzites, and argillites deposited in a glacial environment. The distribution of varved argillites and silty limestones suggests continental and marine facies, respectively. Pebble and ripple-drift orientations, distribution of limestones, striated pavements, distribution of the underlying Bruce Group, and Huronian quartzite

Authors

David A. Lindsey

Geology, Geophysics, and Geochemistry Science Center