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Upper Rideau Lake

  • 6 min read
  • 8 chapters

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Through Lake, Drainage basin and Fault (geology)

Geography

Upper Rideau Lake is bordered by the village of Westport to the west and Newboro to the south.

Hydrology

Upper Rideau Lake is the summit of the Rideau Canal system, with a surface elevation of 124 meters (408 ft) above sea level. Despite having the highest elevation, Upper Rideau Lake is not at the top of the watershed. Water flows north to the Rideau River but does not flow south to the Cataraqui River.

Inflow comes from Westport Sand Lake, part of the Rideau Lake Subwatershed, while outflow winds through the Narrows Lock and into Big Rideau Lake, which eventually flows to the Saint Lawrence River via the Ottawa River.

Geology

The Rideau Lake Fault is a normal fault which exposes granite that can be observed on much of Upper Rideau Lake's northern shore. The northern half of Upper Rideau Lake is located in the Algonquin Highlands. The bedrock in the Precambrian landscape consists mostly of gneiss and marble and is covered in a very thin layer of mixed glacial sediment. The southern half of Upper Rideau Lake is located between the Algonquin Highlands and the Smiths Falls Limestone Plain. The bedrock here consists of Paleozoic quartzose sandstone, dolomite, and conglomerate covered in a variety of sediments: glacial till, silt, clay, organic deposits, and sand.

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