The Fawnie Range is a small hill-range located to the south of the Ootsa Lake reservoir and to the north of the West Road River in the Nechako Plateau region of the Central Interior of British Columbia, Canada. [1] The northwest part of the park is within Entiako Provincial Park and includes Mount Swannell, (1821 m /5974 ft), [2] one of the range's main summits, overlooking Natalkuz Lake (part of the Ootsa Reservoir) from the south. Other named summits include Tutial Mountain (1844 m / 6050 ft), [3] Fawnie Dome (1733 m / 5686 ft) [4] and Fawnie Nose (1933 m / 6342 ft), the highest summit in the range. [5]
Mount Robson is the most prominent mountain in North America's Rocky Mountain range; it is also the highest point in the Canadian Rockies. The mountain is located entirely within Mount Robson Provincial Park of British Columbia, and is part of the Rainbow Range. Mount Robson is the second highest peak entirely in British Columbia, behind Mount Waddington in the Coast Range. The south face of Mount Robson is clearly visible from the Yellowhead Highway, and is commonly photographed along this route.
In the mountaineering parlance of the Western United States, a fourteener is a mountain peak with an elevation of at least 14,000 ft (4267 m). The 96 fourteeners in the United States are all west of the Mississippi River. Colorado has the most (53) of any single state; Alaska is second with 29. Many peak baggers try to climb all fourteeners in the contiguous United States, one particular state, or another region.
The North Shore Mountains are a mountain range overlooking Vancouver in British Columbia, Canada. Their southernmost peaks are visible from most areas in Vancouver and form a distinctive backdrop for the city.
The Rainbow Range is a small subrange of the Park Ranges subdivisions of the Northern Continental Ranges of the Rocky Mountains on the border between Alberta and British Columbia in Mount Robson Provincial Park.
The Dickson Range is a subrange of the Chilcotin Ranges subset of the Pacific Ranges of the Coast Mountains in southwest-central British Columbia. It is located just west of the town of Gold Bridge between the valley of Slim Creek to the north and Downton Lake Reservoir to the south. At its eastern foot is Gun Lake; its western limit is at a pass between Slim Creek and Nichols Creek near the pass which separates the Bridge River basin from that of the Lord River, which feeds the Taseko Lakes.
Monmouth Mountain, commonly known as Mount Monmouth is one of the principal summits of the Pacific Ranges of the Coast Mountains of southern British Columbia. At 3,182 m (10,440 ft), it is the highest summit of the Chilcotin Ranges. It stands just north of the Lillooet Icecap between the heads of Chilko Lake and the Taseko Lakes. West of Chilko Lake's south arm is Mount Good Hope 3,242 m (10,636 ft) and, beyond it, the massif surrounding Mount Queen Bess 3,298 m (10,820 ft), which is the highest summit east of the Homathko River.
Tŝ’ilʔoŝ, also known as Mount Tatlow, is one of the principal summits of the Chilcotin Ranges subdivision of the Pacific Ranges of the Coast Mountains of southern British Columbia. Standing on an isolated ridge between the lower end of Chilko Lake and the Taseko Lakes, it is 3,063 m (10,049 ft) in elevation.
The Black Tusk, known as Q̓elqámtensa ti Skenknápa in the St'at'imcets (Lillooet) language and as T'ákt'akmúten tl'a Ín7inyáx̱a7en in the Sḵwx̱wú7mesh (Squamish) language, is a stratovolcano and a pinnacle of volcanic rock in Garibaldi Provincial Park of British Columbia, Canada. At 2,319 m (7,608 ft) above sea level, the upper spire is visible from a great distance in all directions. It is particularly noticeable from the Sea-to-Sky Highway just south of Whistler, British Columbia. Distinctive and immediately identifiable, The Black Tusk is among the best known mountains in the Garibaldi Ranges of the Coast Mountains. The volcano is part of the Garibaldi Volcanic Belt which is a segment of the Canadian Cascade Arc, but it is not within the geographic boundary of the Cascade Range.
The Hazelton Mountains are a grouping of mountain ranges on the inland lee of the Kitimat Ranges of the Coast Mountains in northwestern British Columbia, Canada, spanning the area of Hazelton south to the Nechako Reservoir. Defined by the British Columbia geographic names office, they span from the Nass River to the Nechako Plateau, and between the Coast Mountains and the Bulkley River, they are considered by geographers to be part of the Interior Mountains complex, though in local perspective they are considered to be part of the Coast Mountains. They are neighboured on the west by the Kitimat Ranges and on the east by the southernmost section of the Skeena Mountains; beyond the Nass River, which is their northern boundary, are the Boundary Ranges of the Coast Mountains. To their southeast is the Nechako Plateau, including the Quanchus Range on the near-island between Ootsa and Eutsuk Lakes of the Nechako Reservoir.
The Fitzsimmons Range is a small mountain range on the northwestern edge of the Garibaldi Ranges in southwestern British Columbia, Canada, located between the valleys of Cheakamus Lake (SW) and Fitzsimmons Creek (NE). Its most famous summit is Whistler Mountain, which overlooks the resort town of Whistler and is one of the two mountains forming the Whistler Blackcomb ski resort. Most of the range is within Garibaldi Provincial Park, while its northeastern extremity is part of the resort municipality, and of the lands associated with the ski resort operation. Other summits in the range include Oboe Summit, Piccolo Summit and Flute Summit, which are hillocks along the ridge running southeast from Whistler Mountain and were named in association with the renaming of Whistler. Beyond them is Singing Pass and Mount Fitzsimmons 2603 m (8540 ft) which is at the opposite end of the range from Whistler Mountain and the location of Fitzsimmons Glacier, which is the source of Fitzsimmons Creek.
Mount Swannell, 1821 m (5974 ft), prominence 771 m, is a mountain in the Fawnie Range of the Nechako Plateau in the Central Interior region of British Columbia, Canada. It is located to the south of the outlet of the Entiako River into Natalkuz Lake, which is part of the Nechako Reservoir. The northernmost of the summits of the Fawnie Range and is in the northeastern end of Entiako Provincial Park, it is the only named summit of the Fawnie Range within the park.
Fawnie Nose is the highest summit of the Fawnie Range of the Nechako Plateau in the Central Interior of British Columbia, Canada. The range is located north of the West Road River and to the south of the Natalkuz Lake portion of the Ootsa Lake reservoir.
The Nechako Range, 1795 km2, is a ridge-like hill-range on the Interior Plateau of the Central Interior of British Columbia, located southwest of the city of Prince George and to the east of the similar Fawnie Range. Formerly known as Nechako Mountain, the range lies between the West Road River to its south and the Euchiniko River to the north, and Knewstubb Lake to its northwest.
Devils Couch is a 2,749-metre (9,019-foot) mountain summit located in the Valhalla Ranges of the Selkirk Mountains in southeast British Columbia, Canada. It is situated in Valhalla Provincial Park, 5 km (3.1 mi) north of Gladsheim Peak, 12 km (7.5 mi) west of Slocan Lake, and 15 km (9.3 mi) northwest of Slocan. The mountain's descriptive name refers to its shape. It was first called "The Toboggan Slide" by early miners who arrived in the area in the 1890s. It was later called "King Tuts Couch" in the 1920s, coinciding with the archaeological discovery in Egypt. This peak's current name was officially adopted July 22, 1964, by the Geographical Names Board of Canada. The peak is located in Devils Range, which is a compact subrange of the Valhallas. The names of the neighboring peaks have a devil-related theme: Black Prince Mountain, Lucifer Peak, Mount Mephistopheles, Devils Dome, Mount Diablo, Satan Peak, and Devils Spire.