Kimsquit Ridge, 1827 m, [1] is a mountain ridge on the west side of the Kimsquit River in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada. It is north of the head of Dean Channel in between Foresight and Robson Creeks. [2] There is a secondary peak, slightly lower than the northern peak, named Whitecone Peak, which is 1823 m elevation. [1] The Bivouac Mountain Encyclopedia has dubbed the northern, slightly higher summit, Bluecone Peak. [3]
Mount Logan is the highest mountain in Canada and the second-highest peak in North America after Denali. The mountain was named after Sir William Edmond Logan, a Canadian geologist and founder of the Geological Survey of Canada (GSC). Mount Logan is located within Kluane National Park Reserve in southwestern Yukon, less than 40 km (25 mi) north of the Yukon–Alaska border. Mount Logan is the source of the Hubbard and Logan glaciers. Although many shield volcanoes are much larger in size and mass, Mount Logan is believed to have the largest base circumference of any non-volcanic mountain on Earth, including a massif with eleven peaks over 5,000 m (16,000 ft). Mount Logan is the 6th most topographically prominent peak on Earth.
Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain on the Great Divide, on the British Columbia/Alberta border in Canada.
Shuswap Lake Marine Provincial Park is a provincial park in British Columbia, Canada, comprising 894 ha. The Park has a variety of amenities including boat launch ramps, picnic areas, and 27 campsites around the perimeter of Shuswap Lake. The lake's name and that of the surrounding Shuswap Country is from the Shuswap people (Secwepemc), the most northern of the Salishan speaking people.
Manastash Ridge is a long anticline mountain ridge located in central Washington state in the United States. Manastash Ridge runs mostly west-to-east in Kittitas and Yakima counties, for approximately 50 miles. The ridge is part of the Yakima Fold Belt of east-tending long ridges formed by the folding of Miocene Columbia River basalt flows.
The Cassiar Mountains are the most northerly group of the Northern Interior Mountains in the Canadian province of British Columbia and also extend slightly into the southernmost Yukon Territory. They lie north and west of the Omineca Mountains, west of the northernmost Rockies and the Rocky Mountain Trench, north of the Hazelton Mountains and east of the Boundary Ranges. They form a section of the Continental Divide, that, in this region, separates water drainage between the Arctic and Pacific Oceans. Physiographically, they are a section of the larger Yukon-Tanana Uplands province, which in turn are part of the larger Intermontane Plateaus physiographic division.
Kimsquit is a former village of the Nuxalk at the mouth of the Dean River on the northeast side of Dean Channel in the Central Coast region of British Columbia, Canada. Kemsquit Indian Reserve No. 1 is nearby at 52°49′00″N126°58′00″W, which is on Kimsquit Bay; Kimsquit Mountain is nearby.
The Whitesail Range is a subrange of the Tahtsa Ranges, located north of Whitesail River in northern British Columbia, Canada.
The Pattullo Range is a subrange of the Hazelton Mountains, located south of Tesla Lake and northeast of Bella Coola in northern British Columbia, Canada. Its highest summit is Tsaydaychuz Peak, 2758 m.
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.
Chatsquot Mountain, 2365 m, is a high-prominence summit in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada, located northwest of Kimsquit Lake, east of the lower Kitlope River, and at the upper end of the basin of the Kimsquit River. It is part of the Kitimat Ranges which in turn form part of the Coast Mountains. With a topographic prominence of 1,981 m (6,499 ft), it is one of Canada's Ultra peaks and is the 98th most prominent summits of North America. It is also one of the most isolated mountain peaks of Canada.
The Kokanee Range is a subrange of the Selkirk Mountains in the West Kootenay region of southeastern British Columbia, Canada. It is located between the valley of the Slocan River (W) and that of Kootenay Lake (E), and to the north of the Kootenay River and the West Arm of Kootenay Lake. The range includes Kokanee Glacier Provincial Park, Kokanee Peak, and Grays Peak, notable as the mountain featured on the label of Kokanee beer. The name "Kokanee" refers to a land-locked variety of Sockeye salmon.
Stein Mountain, elev. 2761 m, is a mountain in the Lillooet Ranges of southwestern British Columbia, Canada, located northwest of the confluence of the Stein and Fraser Rivers, which is just upstream from the town of Lytton. Its name derives from that of the Stein River.
The Kimsquit River is a river in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada, flowing into the head of Dean Channel, one of the major inlets of the Central Coast region.
Chatscah Indian Reserve No. 2, officially Chatscah 2 is an Indian reserve of the Nuxalk Nation band government, located at the mouth of the Kimsquit River at the head of Dean Channel. Like nearby Kimsquit, at the mouth of the Dean River to the southeast, this Indian reserve was one of two reserves set aside of the once-populous Kimsquit subgroup of the Nuxalk, whose surviving post-smallpox population gathered at Bella Coola.
Comet Mountain, 1742 m, is a mountain in the Kitimat Ranges of British Columbia, Canada, located immediately west of the head of Dean Channel in the Central Coast region of that province, to the northwest of the town of Bella Coola. The former Nuxalk village and still-Indian reserve Kimsquit is located immediately east across Dean Channel, Chatscah Indian Reserve No. 2 is immediately north at the mouth of the Kimsquit River.
Kimsquit Peak, 2268 m, is a mountain in the Kitimat Ranges of the Coast Mountains of British Columbia, Canada, located immediately north of the former Nuxalk village of Kimsquit, which is at the mouth of the Dean River. Immediately to its west across the head of Dean Channel is Comet Mountain.
Cornice Peak, 2093 m, is a mountain in the Kitimat Ranges of the Coast Mountains in British Columbia, Canada. It is located on the west side of the Kimsquit River just northwest of the head of Dean Channel. The Kapella River, a tributary of the Kitlope, rises on the west side of Cornice Peak.
Cornice Mountain, 1503 m, is a mountain in the Stikine Icecap area of the Boundary Ranges in northwestern British Columbia, Canada. It is located southwest of the confluence of the Flood and Stikine Rivers.
Mount Jacobsen, 3031 m, is a mountain in the northernmost Pacific Ranges of the Coast Mountains in the Central Coast region of British Columbia, Canada, located to the south of the Bella Coola Valley and immediately south of Ape Lake, to the west of the valley of the Talchako River.