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Lake Temiscaming

 
 
Columbia Encyclopedia: Lake Temiscaming
Temiscaming, Lake, Fr. Témiscamingue, an expansion of the Ottawa River, 121 sq mi (313 sq km), SW Que., Canada, extending 62 mi (100 km) SE from New Liskeard to Temiscaming. The surrounding area is rich in minerals.


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Lake Timiskaming
Lake Timiskaming -
Location Ontario/Quebec
Coordinates 47°20′N 79°30′W / 47.333°N 79.5°W / 47.333; -79.5Coordinates: 47°20′N 79°30′W / 47.333°N 79.5°W / 47.333; -79.5
Lake type Rift lake
Basin  countries Canada
Surface area 295 km2 (114 sq mi)
Max. depth 216 m (710 ft)
Surface  elevation 178.40 m (585.3 ft)[1]
References [1]

Lake Timiskaming (French: Lac Témiscamingue) is a large freshwater lake on the provincial border between Ontario and Quebec, Canada. The lake, which forms part of the Ottawa River, is 110 kilometers (70 mi) in length and covers an area of almost 295 km2 (114 sq mi). Its water level ranges between 175 m (574 ft) and 179 m (587 ft) above sea-level, with a mean annual average of 178.40 m (585.3 ft)[1]. The lake is in places up to 216 m (709 ft) 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 waters".

The lake and surrounding area are popular for outdoor recreation. In June 11, 1978, 12 children and 1 teacher from St. John's School of Ontario (defunct), Toronto, died of hypothermia, when their canoes capsized on a school canoe trip.

There are 30 species of fish in Lake Timiskaming, the best known are northern pike, sturgeon, lake trout, walleye, smallmouth bass, bullhead, carp, ling, 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-Barlow, which existed about 9,500 years ago.

Looking south over Lake Timiskaming from Fort Témiscamingue near Ville-Marie, Quebec.

Lake Timiskaming Rift Valley

Lake Timiskaming is centered on a major rift valley that extends several hundred miles to the north-east called the 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 (3 mi) 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

  1. ^ a b c Ottawa River Regulation Planning Board - Principal Reservoirs Current Water Levels and System Constraints

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Columbia Encyclopedia. The Columbia Electronic Encyclopedia, Sixth Edition Copyright © 2003, Columbia University Press. Licensed from Columbia University Press. All rights reserved. www.cc.columbia.edu/cu/cup/ Read more
Wikipedia. This article is licensed under the Creative Commons Attribution/Share-Alike License. It uses material from the Wikipedia article "Lake Timiskaming" Read more