Tatlatui Lake
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Tatlatui Lake
Tatlatui Lake is a lake in the Tatlatui Range of the Omineca Mountains of the Northern Interior of British Columbia, Canada. It is the source of the Firesteel River, the uppermost left tributary of the Finlay River, which begins just southeast at Thutade Lake, which is considered the ultimate source of the Mackenzie River. The lake and adjoining summits are part of Tatlatui Provincial Park Tatlatui Provincial Park is a provincial park in British Columbia, Canada, located at the southern end of the Spatsizi Plateau and around the headwaters of the Firesteel River, part of the Finlay-Peace River basin and therefore in the Arctic drai .... References Lakes of British Columbia Omineca Mountains Cassiar Land District {{BritishColumbiaInterior-geo-stub ...
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Tatlatui Provincial Park
Tatlatui Provincial Park is a provincial park in British Columbia, Canada, located at the southern end of the Spatsizi Plateau and around the headwaters of the Firesteel River, part of the Finlay-Peace River basin and therefore in the Arctic drainage. Thutade Lake Thutade Lake is located in the Omineca Mountains of the Northern Interior of British Columbia, Canada. About in length, and no more than about wide, the lake is primarily significant as the ultimate source of the Mackenzie River. The lake i ..., at the head of the Firesteel and to the southeast of the park, is considered the ultimate source of the Mackenzie River (via the Finlay and Peace Rivers). References * Provincial parks of British Columbia Stikine Country {{BritishColumbia-park-stub ...
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British Columbia Interior
, settlement_type = Region of British Columbia , image_skyline = , nickname = "The Interior" , subdivision_type = Country , subdivision_name = , subdivision_type1 = Province , subdivision_name1 = , parts_type = Principal cities , p1 = Kelowna , p2 = Kamloops , p3 = Prince George , p4 = Vernon , p5 = Penticton , p6 = West Kelowna , p7 = Fort St. John , p8 = Cranbrook , area_blank1_title = 14 Districts , area_blank1_km2 = 669,648 , area_footnotes = , elevation_max_m = 4671 , elevation_min_m = 127 , elevation_max_footnotes = Mt. Fairweather , elevation_min_footnotes = Fraser River , population_as_of = 2016 , population = 961,155 , population_density_km2 ...
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Firesteel River (Canada)
The Firesteel River is the uppermost left tributary of the Finlay River in the Northern Interior of British Columbia, Canada. The river originates at Tatlatui Lake, while the Finlay originates at the outlet of Thutade Lake, to the southeast, which is considered the ultimate source of the Mackenzie River. See also *Tatlatui Range *Tatlatui Provincial Park *List of British Columbia rivers The following is a partial list of rivers of British Columbia, organized by watershed. Some large creeks are included either because of size or historical importance (See Alphabetical List of British Columbia rivers ). Also included are lakes th ... References Rivers of the Omineca Mountains {{BritishColumbiaInterior-river-stub ...
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Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the la ...
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Tatlatui Range
The Tatlatui Range is a large and very alpine mountain range on the east flank of the upper Skeena River in northern British Columbia, Canada. It has an area of 2307 km2 and is a subrange of the Omineca Mountains which in turn form part of the Interior Mountains.Tatlatui Range
in the Canadian Mountain Encyclopedia The range features several lakes, the largest of which, , is at the head of the , and is considered the ultimate source of the Mackenzie River.

Omineca Mountains
The Omineca Mountains, also known as "the Ominecas", are a group of remote mountain ranges in the Boreal Cordillera of north-central British Columbia, Canada. They are bounded by the Finlay River on the north, the Rocky Mountain Trench (here filled by Lake Williston) on the east, the Nation Lakes on the south, and the upper reaches of the Omineca River on the west. They form a section of the Continental Divide, that, in this region, separates water drainage between the Arctic and Pacific Oceans. The lower course of the Omineca River flows through the heart of the range. To the south of the Ominecas is the Nechako Plateau, to the west the Skeena Mountains and Hazelton Mountains, to the north the Spatsizi Plateau and the Stikine Ranges, while east across the Rocky Mountain Trench are the Muskwa Ranges. "The Omineca" or "the Omineca Country" is the entire area plus some of the northern Nechako Plateau adjacent to the Ominecas, where there has been more settlement and, in the past, ...
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Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ...
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Finlay River
The Finlay River is a 402 km long river in north-central British Columbia flowing north and thence south from Thutade Lake in the Omineca Mountains to Williston Lake, the impounded waters of the Peace River formed by the completion of the W.A.C. Bennett Dam in 1968. Prior to this, the Finlay joined with the Parsnip River to form the Peace. The headwaters of the Finlay at Thutade Lake are considered the ultimate source of the Mackenzie River.''Atlas of Canada: Rivers of Canada'' page
is located just north of Williston Lake. The Finlay drains an area of 43,000 square kilometres and discharges at a mean rate of 600 cubic metres per second. Majo ...
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Thutade Lake
Thutade Lake is located in the Omineca Mountains of the British Columbia Interior, Northern Interior of British Columbia, Canada. About in length, and no more than about wide, the lake is primarily significant as the ultimate source of the Mackenzie River. The lake is at the head of the Finlay River, which joins the Peace River (Canada), Peace River via Williston Lake. The area is very remote, being located about north of Smithers, British Columbia, Smithers, although several mining operations for ores containing copper, lead, zinc and silver have occurred around the lake. The largest of these is the Kemess Mine, an iron and copper property originally owned by Royal Oak Mines and now by Northgate Minerals, located in the valley of Kemess Creek, which is off the northeast end of Thutade Lake. The mine is accessed by the Omineca Resource Road and other resource routes, and is by road from Prince George, British Columbia, Prince George. Just downstream from the outlet of Thu ...
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Lakes Of British Columbia
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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