| Lake Timiskaming | |
| Other Name: | Lake Temiskaming |
| Pushpin Map: | Ontario |
| Location: | Timiskaming District / Nipissing District, Ontario and Témiscamingue Regional County Municipality, Quebec |
| Coords: | 47.3333°N -109°W |
| Type: | Rift lake |
| Inflow: | Blanche River, Ottawa River, Montreal River, Matabitchuan River |
| Outflow: | Ottawa River |
| Basin Countries: | Canada |
| Length: | 110km (70miles) |
| Area: | 295km2 |
| Max-Depth: | 216m (709feet) |
| Elevation: | 178.4m (585.3feet) |
| Islands: | du Collège, MannFarr Island |
| Cities: | Temiskaming ShoresVille-Marie, QuebecVille-Marie, QuebecNotre dam Du Nord |
| Reference: | [1] |
Lake Timiskaming or Lake Temiskaming (French: Lac Témiscamingue) is a large freshwater lake on the provincial boundary between Ontario and Quebec, Canada. The lake, which forms part of the Ottawa River, is 110km (70miles) in length and covers an area of almost 2950NaN0. Its water level ranges between 1750NaN0 and 1790NaN0 above sea-level, with a mean annual average of 178.40NaN0.[1] The lake is in places up to 2160NaN0 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.
Lake Timiskaming is located within an ancient 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 50NaN0 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.[2]