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.
|Lake type||former lake|
|Etymology||Iroquois or Haudenosaunee (/ˈhoʊdənoʊˈʃoʊni/; "People of the Longhouse")|
|Primary inflows||Niagara River|
|Primary outflows||Mohawk River to the Hudson River|
|Max. length||196 mi (315 km)|
|Max. width||57 mi (92 km)|
|Surface elevation||345 ft (105 m)|
|References||United States Geological Survey, George Otis Smith, Director; The Pleistocene of Indiana and Michigan and the History of the Great Lakes; Frank Leverett and Frank B. Taylor; Department of the Interior, Monographs of the United States Geological Survey; Volume LIII; Washington; Government Printing Office; 1915|
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. In Mississauga, the shoreline is found south of Dundas Street and most visible with hills found east and west of Mavis Road.
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.
- Beauchamp, William Martin (1905). A History of the New York Iroquois. New York State Education Department. p. 165. Retrieved May 7, 2016.
- Richard Foster Flint (2008). Glacial Geology and the Pleistocene Epoch. ISBN 978-1-4437-2173-8.
- Larson, Grahame; Schaetzl, Randall (2001). "Review: Origin and Evolution of the Great Lakes" (PDF). J. Great Lakes Res. 27 (4): 518–546. doi:10.1016/S0380-1330(01)70665-X. Archived from the original (PDF) on 2008-10-31. The work of Anderson and Lewis (1985) is the basis for these authors' views on the history of the postglacial water levels.
- Donnelly, Jeffrey P.; Neal W. Driscoll; Elazar Uchupi; Lloyd D. Keigwin; William C. Schwab; E. Robert Thieler; Stephen A. Swift (February 2005). "Catastrophic meltwater discharge down the Hudson Valley: A potential trigger for the Intra-Allerød cold period". Geology. 33 (2): 89–92. Bibcode:2005Geo....33...89D. doi:10.1130/G21043.1.
- Eyles, Nick (2002). Ontario Rocks: Three Billion Years of Environmental Change. Markham, Ontario: Fitzhenry & Whiteside. ISBN 9781550416190. OCLC 48940760. See chapter 17.
- "Nearshore Geology". City of Toronto TRC. n.d. Archived from the original on 26 February 2012. Retrieved 26 December 2009.
- Tesmer, Irving H.; Bastedo, Jered C. (1981). Colossal cataract: the geologic history of Niagara Falls. p. 48. ISBN 978-0-87395-522-5. Retrieved 2 February 2010.