Glacial Lake Iroquois
Glacial Lake Iroquois was a prehistoric proglacial lake that existed at the end of the last ice age approximately 13,000 years ago. The lake was essentially an enlargement of the present Lake Ontario that formed because the St. Lawrence River downstream from the lake was blocked by the ice sheet near the present Thousand Islands. The level of the lake was approximately 30 m (~100 ft) above the present level of Lake Ontario.
The lake drained to the southeast, through a channel passing near present day Rome, New York. The Rome Sand Plains has several sand ridges that geologists think were formed at this time. The channel then followed the valley of the Mohawk River to the Hudson River.
The lake was fed by Early Lake Erie, as well as Glacial Lake Algonquin, an early partial manifestation of Lake Huron, that drained directly to Lake Iroquois across southern Ontario, along the southern edge of the ice sheet, bypassing Early Lake Erie.
Two ancient shorelines in the Toronto area mark the existence of former glacial lakes. About 2 km inland from the shore a ridge known as the Iroquois Shoreline can be discerned. The old shoreline runs west-east running roughly parallel to Davenport Road just south of St. Clair Avenue West. Further east, the Scarborough Bluffs also formed part of the shoreline of the ancient lake.
Another ancient shoreline exists between 2–4 km offshore of Toronto. It is known as the Toronto Scarp and formed the shore of Glacial Lake Warren or Admiralty Lake. From Bluffer's Park in Scarborough to just west of Hanlan's Point is an underwater bluff.
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- Larson, Grahame; Schaetzl, Randall (2001). "Review: Origin and Evolution of the Great Lakes". J. Great Lakes Res. 27 (4): 518–546. The work of Anderson and Lewis (1985) is the basis for these authors' views on the history of the postglacial water levels.
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- History of Lake Iroquois
- Lake Iroquois and its shore cliff, showing map of the lake
- Deglaciation of the Central St. Lawrence Lowland