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Lake Timiskaming

Freshwater lake in Canada


Freshwater lake in Canada

FieldValue
nameLake Timiskaming
other_nameLake Temiskaming
native_namefr
imageTemiskaming Lake.jpg
pushpin_mapOntario
locationTimiskaming District / Nipissing District, Ontario and Témiscamingue Regional County Municipality, Quebec
coords
typeRift lake
inflowBlanche River, Ottawa River, Montreal River, Matabitchuan River
outflowOttawa River
basin_countriesCanada
length110 km
area304 km2
{{convert122mftabbron}}
max-depth216 m
{{convert37.09km3cumiabbron}}
elevation178.40 m
islandsdu Collège, Mann
citiesTemiskaming Shores
reference
Note

the lake

122 m | max-depth = 216 m 37.09 km3 Farr Island Ville-Marie, Quebec Ville-Marie, Quebec Notre dam Du Nord

**Lake Timiskaming ** or Lake Temiskaming (, ) is a large freshwater lake on the provincial boundary between Ontario and Quebec, Canada. The lake, which forms part of the Ottawa River, is 110 km in length and covers an area of 304 km2. Its water level ranges between 175 m and 179 m above sea-level, with a mean annual average of 178.4 m. The lake is in places up to 216 m deep. There are several islands on the lake, notably Mann and du Collège Islands.

The name is from the Algonquin Temikami or Temikaming, meaning "deep body of water with rapid winds”

There are 30 species of fish in Lake Timiskaming, the best known are northern pike, sturgeon, lake trout, walleye, smallmouth bass, bullhead, carp, burbot, perch, and whitefish.

The lake was shaped during the last ice age when glaciers carved into the rock. It is also the remnants of a huge basin called Lake Ojibway, which existed about 9,500 years ago.

For the trading post and some history see Fort Témiscamingue.

One of Canada's greatest boating tragedies occurred when twelve boys and a staff member of Ted Byfield's St John's School of Claremont died of drowning and hypothermia on a canoe trip on 11 June 1978 on the lake.

Timiskaming Graben

Lake Timiskaming is located within the ancient major rift valley Timiskaming Graben. It is the northern extension of the Ottawa-Bonnechere Graben, which is part of the Saint Lawrence rift system.

There have been recent earthquakes along the rift valley, the most recent being in 2000. There are numerous faults in the area and has produced cliffs such as Devil's Rock, just 5 km south of Haileybury and is dated to be 2.2 billion years old. There are known kimberlite pipes within the rift valley that are considered to be diamondiferous.

References

References

  1. [https://www.thecanadianencyclopedia.ca/en/article/timiskaming-lake Timiskaming Lake], on ''thecanadianencyclopedia.ca''
  2. [https://www.thecanadianencyclopedia.ca/en/article/timiskaming-lake Timiskaming Lake], on ''thecanadianencyclopedia.ca''
  3. [https://www.thecanadianencyclopedia.ca/en/article/timiskaming-lake Timiskaming Lake], on ''thecanadianencyclopedia.ca''
  4. [http://www.ottawariver.ca/emain.htm Ottawa River Regulation Planning Board – Principal Reservoirs Current Water Levels and System Constraints] {{webarchive. link. (2008-12-05)
  5. (13 June 2019). "History Through Our Eyes: June 13, 1978, canoe trip tragedy". The Gazette.
  6. Sader, Jamil Andrei. (2004-01-01). "Low temperature serpentinization processes and kimberlite groundwater signatures in the Kirkland Lake and Lake Timiskiming kimberlite fields Ontario, Canada". The University of Texas at Dallas.
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