Strange, Ontario - Ecology

Ecology

The Strange Till Plain is a flat ground moraine with underlying glacial till. It was formed by the Ontario ice lobe during the Port Huron Stadial. It is believed that this till plain exhibits the original surface; very little erosion or surface deposition is observable throughout its 3 square kilometre range.

This Till plain is located between and within the Albion and Uxbridge wedges of the Oak Ridges Moraine, and is a constituent part of that moraine.

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