The Rancheria River is a tributary of the Liard River in the southern Yukon Territory, Canada, just north of the border with British Columbia. The river's main tributary is the Little Rancheria River, which begins in British Columbia. Both river basins are in the northernmost of extension of the Stikine Ranges of the Cassiar Mountains, which extend from the Finlay River north to the Liard and end just inside the Yukon, with the Rancheria River forming the northern end of the range.
A tributary or affluent is a stream or river that flows into a larger stream or main stem river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean.
The Liard River flows through Yukon, British Columbia and the Northwest Territories, Canada. Rising in the Saint Cyr Range of the Pelly Mountains in southeastern Yukon, it flows 1,115 kilometres (693 mi) southeast through British Columbia, marking the northern end of the Rocky Mountains and then curving northeast back into Yukon and Northwest Territories, draining into the Mackenzie River at Fort Simpson, Northwest Territories. The river drains approximately 277,100 square kilometres (107,000 sq mi) of boreal forest and muskeg.
British Columbia is the westernmost province of Canada, located between the Pacific Ocean and the Rocky Mountains. With an estimated population of 5.016 million as of 2018, it is Canada's third-most populous province.
The Stikine River is a river, historically also the Stickeen River, approximately 610 km (379 mi) long, in northwestern British Columbia in Canada and in southeast Alaska in the United States.
Dease Lake is a small community located in the Cassiar Country of the Northern Interior of British Columbia, Canada. Located a few hours south of the Yukon border, it is located on Stewart–Cassiar Highway at the south end of the lake of the same name. Dease Lake is the last major centre before the Alaska Highway, and also the junction to Telegraph Creek and the Grand Canyon of the Stikine. Dease Lake Indian Reserve No. 9 is located nearby and is under the governance of the Tahltan First Nation band government.
The Rocky Mountain Trench, also known as The Valley of a Thousand Peaks or simply the Trench, is a large valley on the western side of the northern part of North America's Rocky Mountains. The Trench is both visually and cartographically a striking physiographic feature extending approximately 1,600 km (1,000 mi) from Flathead Lake, Montana to the Liard River, just south of the British Columbia-Yukon border near Watson Lake, Yukon. The trench bottom is 3-16 km wide and ranges from 600-900 metres above sea level. The general orientation of the Trench is an almost uniform 150/330 degree geographic north vector and has become convenient as a visual guide for aviators heading north or south.
The Boundary Ranges, also known in the singular and as the Alaska Boundary Range, are the largest and most northerly subrange of the Coast Mountains. They begin at the Nass River, near the southern end of the Alaska Panhandle in the Canadian province of British Columbia and run to the Kelsall River, near the Chilkoot Pass, beyond which are the Alsek Ranges of the Saint Elias Mountains, and northwards into the Yukon Territory flanking the west side of the Yukon River drainage as far as Champagne Pass, north of which being the Yukon Ranges. To their east are the Skeena Mountains and Stikine Plateau of the Interior Mountains complex that lies northwest of the Interior Plateau; the immediately adjoining subregion of the Stikine Plateau is the Tahltan Highland. To their northeast is the Tagish Highland, which is a subregion of the Yukon Plateau. Both highlands are considered in some descriptions as included in the Coast Mountains. The Alexander Archipelago lies offshore and is entirely within Alaska.
John McLeod was a Scottish-born explorer of Canada, in his capacity as a fur trader with the North West Company and Hudson's Bay Company. He is remembered primarily for his explorations of several major rivers of the southwestern Northwest Territories, southern Yukon Territory, and northern British Columbia.
The Stikine Ranges are a group of mountain ranges and mountainous plateaus in northwestern British Columbia, Canada. They are the northernmost subdivision of the Cassiar Mountains and among the least explored and most undeveloped parts of the province.
The Tuya Range is a rmountain range in the Stikine Ranges of the Cassiar Mountains in the far north of the Canadian province of British Columbia, near its border with the Yukon Territory and to the southwest of Watson Lake, Yukon, which is the nearest major settlement.
Toozaza Peak is a tuya in the Stikine Ranges of the Cassiar Mountains in northern British Columbia, Canada, located in the Iverson Creek. Toozaza Peak is the summit of a north-south aligned ridge between the head of Toozaza Creek and the head of the Jennings River, just south of the Jennings' divide with the Little Rancheria River headwaters. The Little Rancheria and Toozaza Creek are part of the Liard, while the Jennings is part of the Yukon River drainage via Teslin Lake, and the peak therefore stands astride the line of the Continental Divide. It is part of the Tuya Volcanic Field, a volcanic field associated with the Stikine Volcanic Belt, part of the Northern Cordilleran Volcanic Province.
The Stikine Country, also referred to as the Stikine District or simply "the Stikine", is one of the historical geographic regions of the Canadian province of British Columbia, located inland from the central Alaska Panhandle and comprising the basin of the Stikine River and its tributaries. The term Stikine–Iskut is also fairly common to describe the area, and references the Iskut River, the Stikine's largest tributary and describable as its south fork.
Rancheria River may refer to:
The Beaver River is a tributary of the Liard River, entering that stream in the area of its Grand Canyon just south of the British Columbia-Yukon border after running generally south-east from its origin in the extreme southeast corner of the Yukon Territory.
The Stikine Plateau is a plateau in northern British Columbia, Canada. It lies between the Boundary Ranges of the Coast Mountains on the west and southwest and the Cassiar Mountains along its northeast, and between the Skeena Mountains on its south and southeast and the Jennings and Nakina Rivers on the north.
The Little Rancheria River is a tributary of the Rancheria River having its origin in the northernmost Stikine Ranges of British Columbia, Canada, and joining its parent stream in the Yukon Territory. The Rancheria is a tributary of the Liard and defines the northern limit of the Stikine Ranges and their parent range, the Cassiar Mountains. The river crosses the provincial-territorial boundary at 129° 48' 00" W.
The Jennings River is a river in far northern British Columbia, Canada. It is approximately 150 kilometres (93 mi) long.
The Frog Lakes are a group of lakes, drained eastward by an unnamed stream feeding the Frog River, a tributary of the Kechika River in the Stikine Ranges of the Northern Interior of British Columbia. Though not the hydrological source of the Frog River, the lakes are notably located in an east-west aligned valley which forms the divide between the basins of the Stikine River and that of the Liard, and are therefore located on the Continental Divide between the Pacific and Arctic drainages. Draining from their west is the Pitman River, a Stikine tributary, from an unnamed lake just to their west( which also drains east to feed the Frog Lakes themselves), while the Kechika is a major tributary of the Liard, which is a tributary of the Mackenzie. The Frog Lakes Pass, as dubbed by the Canadian Mountain Encyclopedia and at an elevation of 1015 m (3330 ft), is the prominence col for 2668 m (8753 ft) Sharktooth Mountain, giving it a prominence of 1653m.
The Cottonwood River is a tributary of the Dease River in the Cassiar Country of the Northern Interior of British Columbia, Canada. Rising in the northern Stikine Ranges just east of Toozaza Peak, and just south of the origins of the Jennings and Little Rancheria River near the border with Yukon, it flows south along the east flank of the Tuya Range to meet the Dease just north of that river's source at Dease Lake, between the north end of that lake and McDame Creek and the former mining centre and community of McDame Post.
The Klappan River is a major tributary of the Stikine River in northwestern British Columbia, Canada. It flows north from an area known as the Sacred Headwaters, which is the source not only of this river but also of the Nass, Skeena, Spatsizi and Stikine Rivers. The headwaters region is the site of a controversial coal-bed methane project.
The Stikine Region is an unincorporated area in northwesternmost British Columbia, Canada and is the only area in B.C. not in a regional district. The Stikine Region was left unincorporated following legislation that established the province's regional districts in 1968 and is not classified as a regional district. It contains no municipal governments which normally constitute the majority of seats on the boards of regional districts. There is only one local planning area, the Atlin Community Planning Area, which was combined in 2009 with the Atlin Community Improvement District to provide fire, landfill, water, streetlighting, sidewalks and advisory land use services. All other services not provided privately are administered directly by various provincial government ministries. The area around Dease Lake, formerly in the Stikine Region, is now within the boundaries of the Regional District of Kitimat-Stikine following a boundary amendment in 2008.
The BC Geographical Names is a geographic name web service and database for the Canadian province of British Columbia run by the Base Mapping and Geomatic Services Branch of the Integrated Land Management Bureau. The database contains official names and spellings of towns, mountains, rivers, lakes, and other geographic places. The database often has other useful information, such as the history of geographic names, and their use in history.
Coordinates: 60°13′21″N129°08′40″W / 60.22250°N 129.14444°W
A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.
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