The marsh scape project
the lower oxtongue river, lake of bays, ontario, canada
The Oxtongue River flows from Algonquin Park to Lake of Bays following a glacial outwash channel created by the melting Algonquin glacier. The Lower Oxtongue begins below Marsh’s Falls where it becomes a slow, meandering river winding its way to meet the lake. Over 10,000 years the river has cut different routes through an alluvial floodplain leaving several oxbows and meanders along its length. Glaciofluvial sand terraces and bedrock bound river’s course to the lake. A veritable museum of glacial change, they create an isolated valley of undisturbed natural cover in a region under heavy pressure from cottage development.