Glacial Lake Iroquois

Coordinates: 43°42′N 77°54′W / 43.7°N 77.9°W / 43.7; -77.9
Source: Wikipedia, the free encyclopedia.
Lake Iroquois
Primary inflows
Niagara River
Welland Canal
Primary outflowsMohawk River to the Hudson River
Basin countriesCanada
United States
Max. length196 mi (315 km)
Max. width57 mi (92 km)
Surface elevation345 ft (105 m)
ReferencesUnited 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

Glacial Lake Iroquois was a prehistoric proglacial lake that existed at the end of the last ice age approximately 13,000 years ago.[2] 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.[3]

Stages of great lake development.

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.[3]

The lake was fed by

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.

The subsequent melting of the ice dam resulted in a sudden lowering of the lake to its present level, a potential trigger for the Younger Dryas episode.[4]

Remnant shorelines

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.[5] In Mississauga, the shoreline is found south of Dundas Street and most visible with hills found east and west of Mavis Road.[6]

Another ancient shoreline exists between 2–4 km offshore of Toronto. It is known as the

Admiralty Lake. From Bluffer's Park in Scarborough to just west of Hanlan's Point is an underwater bluff.[7]

In New York, Ridge Road and New York State Route 104 run from west to east along a ridge of the old shoreline of Lake Iroquois.[8]

See also

References

  1. ^ Beauchamp, William Martin (1905). A History of the New York Iroquois. New York State Education Department. p. 165. Retrieved May 7, 2016.
  2. ^ Richard Foster Flint (2008). Glacial Geology and the Pleistocene Epoch. Read Books.
    ISBN 978-1-4437-2173-8
    .
  3. ^
    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.
  4. doi:10.1130/G21043.1
    .
  5. OCLC 48940760
    . See chapter 17.
  6. ^ "Natural Areas Survey (NAS) Site: ER6" (PDF). mississauga.ca. Retrieved 2023-07-10.
  7. ^ "Nearshore Geology". City of Toronto TRC. n.d. Archived from the original on 26 February 2012. Retrieved 26 December 2009.
  8. ISBN 978-0-87395-522-5
    . Retrieved 2 February 2010.

External links
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