The Rocky Mountains, also known as the Rockies, are a major mountain range and the largest mountain system in North America. The Rocky Mountains stretch 3,000 miles in straight-line distance from the northernmost part of western Canada, to New Mexico in the southwestern United States. Depending on differing definitions between Canada and the U.S., its northern terminus is located either in northern British Columbia's Terminal Range south of the Liard River and east of the Trench, or in the northeastern foothills of the Brooks Range/British Mountains that face the Beaufort Sea coasts between the Canning River and the Firth River across the Alaska-Yukon border. Its southernmost point is near the Albuquerque area adjacent to the Rio Grande rift and north of the Sandia–Manzano Mountain Range. Being the easternmost portion of the North American Cordillera, the Rockies are distinct from the tectonically younger Cascade Range and Sierra Nevada, which both lie farther to its west.
Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain on the Great Divide, on the British Columbia/Alberta border in Canada.
Mount Bryce is a mountain at the southwestern corner of the Columbia Icefield, in British Columbia, Canada, near the border with Alberta. It can be seen from the Icefields Parkway.
The Selkirk Mountains are a mountain range spanning the northern portion of the Idaho Panhandle, eastern Washington, and southeastern British Columbia which are part of a larger grouping of mountains, the Columbia Mountains. They begin at Mica Peak and Krell Hill near Spokane and extend approximately 320 km north from the border to Kinbasket Lake, at the now-deserted location of the onetime fur company post, Boat Encampment. The range is bounded on its west, northeast and at its northern extremity by the Columbia River, or the reservoir lakes now filling most of that river's course. From the Columbia's confluence with the Beaver River, they are bounded on their east by the Purcell Trench, which contains the Beaver River, Duncan River, Duncan Lake, Kootenay Lake and the Kootenay River. The Selkirks are distinct from, and geologically older than, the Rocky Mountains. The neighboring Monashee and Purcell Mountains, and sometimes including the Cariboo Mountains to the northwest, are also part of the larger grouping of mountains known as the Columbia Mountains. A scenic highway loop, the International Selkirk Loop, encircles the southern portions of the mountain range.
The Chilcotin Ranges are a subdivision of the Pacific Ranges of the Coast Mountains. They lie on the inland lea of the Pacific Ranges, abutting the Interior Plateau of British Columbia. Their northwestern end is near the head of the Klinaklini River and their southeast end is the Fraser River just north of Lillooet; their northern flank is the edge of the Plateau while their southern is the north bank of the Bridge River. In some reckonings they do not go all the way to the Fraser but end at the Yalakom River, which is the North Fork of the Bridge.
Greenwood is a city in south central British Columbia. It was incorporated in 1897 and was formerly one of the principal cities of the Boundary Country smelting and mining district. It was incorporated as a city originally and has retained that title despite the population decline following the closure of the area's industries.
Hoodoo Mountain, sometimes referred to as Hoodoo Volcano, is a potentially active stratovolcano in the Northern Interior of British Columbia, Canada. It is located 25 kilometres northeast of the Alaska–British Columbia border on the north side of the Iskut River opposite of the mouth of the Craig River. With a summit elevation of 1,850 metres and a topographic prominence of 900 metres, Hoodoo Mountain is one of many prominent peaks within the Boundary Ranges of the Coast Mountains. Its flat-topped summit is covered by an ice cap more than 100 metres thick and at least 3 kilometres in diameter. Two valley glaciers surrounding the northwestern and northeastern sides of the mountain have retreated significantly over the last hundred years. They both originate from a large icefield to the north and are the sources of two meltwater streams. These streams flow along the western and eastern sides of the volcano before draining into the Iskut River.
The Boundary Country is a historical designation for a district in southern British Columbia lying, as its name suggests, along the boundary between Canada and the United States. It lies to the east of the southern Okanagan Valley and to the west of the West Kootenay. It is often included in descriptions of both of those regions but historically has been considered a separate region. Originally inclusive of the South Okanagan towns of Osoyoos and Oliver, today the term continues in use to refer to the valleys of the Kettle, West Kettle, and Granby Rivers and of Boundary and Rock Creeks and that of Christina Lake and of their various tributaries, all draining the south slope of the Monashee Mountains. The term Boundary District as well as the term Boundary Country can both refer to the local mining division of the British Columbia Ministry of Mines, Energy and Petroleum Resources.
Cinder Mountain is a partly eroded cinder cone at the head of Snippaker Creek, British Columbia, Canada. It is one of the Iskut-Unuk River Cones and is the source of a basaltic lava flow that extends 4 km (2 mi) north into Copper King Creek. An isolated pile of subaerial basalt flows and associated pillow lava rest on varved clay and till in King Creek. Cinder Mountain last erupted during the Pleistocene.
The Similkameen Country, also referred to as the Similkameen Valley or Similkameen District, but generally referred to simply as The Similkameen or more archaically, Similkameen, is a region roughly coinciding with the basin of the river of the same name in the Southern Interior of British Columbia. The term "Similkameen District" also refers to the Similkameen Mining District, a defunct government administrative district, which geographically encompasses the same area, and in more casual terms may also refer to the Similkameen electoral district, which was combined with the Grand Forks-Greenwood riding by the time of the 1966 election. The Similkameen Country has deep historical connections to the Boundary Country and the two are sometimes considered one region, partly as a result of the name of the electoral district. It is also sometimes classed as being part of the Okanagan region, which results from shared regional district and other administrative boundaries and names. The term "Similkameen District" may also historically refer to the Similkameen Division Yale Land District, which also includes Osoyoos and the Boundary Country to Osoyoos' east.
The Kemess Mine was an open-pit copper and gold mine, located just northeast of the foot of Thutade Lake, at the head of the Finlay River, in the Omineca Mountains of the Northern Interior of British Columbia, Canada. It was operated by Royal Oak Mines from 1998 to 1999, when it was bought by Northgate Minerals. Northgate operated the mine until its closure in 2011; that year Northgate was taken over by AuRico Gold. In 2014 AuRico Gold partitioned off its portion of Kemess Mine ownership creating a new company called AuRico Metals.
Copper Mountain was an important copper-mining company town in the Similkameen Country of the Southern Interior of British Columbia, Canada, just south of the town of Princeton.
Allenby was an important copper-mining company town in the Similkameen Country of the Southern Interior of British Columbia, Canada, ten miles south of the town of Princeton adjacent to the Similkameen River. The underground mine worked the seams at elevation in Copper Mountain on the east bank of the river. The mining camp was up on the mountain while the concentrator at Allenby was lower down near the river. It was for a short time the location of the Copper Mountain post office but that name was reinstated to its original site when the neighbouring Copper Mountain mining town, affiliated with the same mine, was revived. The underground mine was in operation from 1917 to 1957 when a new open pit mine opened on the bench up on the west side of the river, confusingly it is also called Copper Mountain. The east bank site has been reworked with an open pit mine after the year 2000.
The Fraser Pass is a mountain pass in the British Columbian Rockies of Western Canada. Its summit is 2,015 m (6,611 ft) above sea level. Although immediately adjacent to the Continental Divide, the pass does not cross it; rather, it bridges the drainage basins of the Fraser River and Columbia River, both Pacific-draining rivers.
Anaconda is an unincorporated community south of the confluence of Eholt and Boundary creeks in the Boundary Country region of south central British Columbia. About 43 kilometres (27 mi) west of Grand Forks, and 82 kilometres (51 mi) east of Osoyoos, on Highway 3, the neighbourhood is immediately south of Greenwood.
Mount Ulysses, is the highest mountain in the Muskwa Ranges of the Northern Canadian Rockies in British Columbia. It and neighbouring peaks are part of a group of names drawing on the epic poem The Odyssey, in which here Ulysses wanders for 10 years before being able to return home to Ithaca.
Tilia johnsoni is an extinct species of flowering plant in the family Malvaceae that, as a member of the genus Tilia, is related to modern lindens. The species is known from fossil leaves found in the early Eocene deposits of northern Washington state, United States and a similar aged formation in British Columbia, Canada.
Sassafras hesperia is an extinct species of flowering plant in the family Lauraceae.
Ulmus okanaganensis is an extinct species of flowering plant in the family Ulmaceae related to the modern elms. The species is known from fossil leaves, flowers, and fruits found in the early Eocene deposits of northern Washington state, United States and similar aged formations in British Columbia, Canada.
The Eocene Okanagan Highlands or Eocene Okanogan Highlands are a series of Early Eocene geological formations which span a 1,000 km (620 mi) transect of British Columbia, Canada, and Washington state, United States. Known for a highly diverse and detailed plant and animal paleobiota the paleolake beds as a whole are considered one of the great Canadian Lagerstätten. The paleobiota represented are of an upland subtropical to temperate ecosystem series immediately after the Paleocene–Eocene thermal maximum, and before the increased cooling of the middle and late Eocene to Oligocene. The fossiliferous deposits of the region were noted as early as 1873, with small amounts of systematic work happening in the 1870–1920s on British Columbian sites, and 1920–1930s for Washington sites. Focus and more detailed descriptive work on the Okanagan Highland sites started in the late 1960s.
