| Strata Range | |
|---|---|
 | |
| Geography | |
| Country | Canada |
| Province | British Columbia |
| Range coordinates | 56°24′N129°05′W / 56.400°N 129.083°W |
| Parent range | Skeena Mountains |
The Strata Range is a subrange of the Skeena Mountains located between the Bell-Irving River and the Taylor River in northern British Columbia, Canada.
The Ridge-and-Valley Appalachians, also called the Ridge and Valley Province or the Valley and Ridge Appalachians, are a physiographic province of the larger Appalachian Highlands division. The physiographic province is divided into three sections: the Hudson Valley, the Central, and the Tennessee.
Mount Rundle is a mountain in Canada's Banff National Park overlooking the towns of Banff and Canmore, Alberta. The Cree name was Waskahigan Watchi or house mountain. In 1858 John Palliser renamed the mountain after Reverend Robert Rundle, a Methodist invited by the Hudson's Bay Company to do missionary work in western Canada in the 1840s. He introduced syllabics there—a written language developed for the Cree, as part of his missionary work. He only visited the Stoney-Nakoda of the area around what is now called Mount Rundle in 1844 and 1847.
The Bare Range is a mountain range of the Canadian Rockies, located south of the Red Deer River valley in Banff National Park, Canada. The range is named for the "bareness" of or lack of trees on the gentle slopes of the range.
The Mackenzie Mountains are a Canadian mountain range forming part of the Yukon–Northwest Territories boundary between the Liard and Peel rivers. The range is named in honour of Canada's second prime minister, Alexander Mackenzie. Nahanni National Park Reserve and Nááts'ihch'oh National Park Reserve are in the Mackenzie Mountains.
The Beaverfoot Range is a mountain range of the Canadian Rockies, located in southeastern British Columbia. The range extends from Cedared Creek near Spillimacheen north to the Kicking Horse River.
The Palliser Range is a mountain range of the Canadian Rockies that lies in the extreme southeast corner of Banff National Park, Alberta, Canada.
The Massive Range is a mountain range of the Canadian Rockies, located in the southwestern area of the Bow River valley in Banff National Park, Canada.
The Skeena Mountains, also known as the Skeenas, are a subrange of the Interior Mountains of northern British Columbia, Canada, essentially flanking the upper basin of the Skeena River. They lie just inland from the southern end of the Boundary Ranges of the Coast Mountains, and also of the northern end of the Kitimat Ranges. Their southern limit is described by the Bulkley River and the upper northwestern reaches of Babine and Takla Lakes, and on their northeast by the upper reaches of the Omineca River.
The Belcher Mountains are a former mountain range that stood in the Hudson Bay region of Canada in the late Precambrian. The mountains have since been uplifted and folded erosion has beveled them into a nearly flat plain.
The Interior Mountains or Northern Interior Mountains are the semi-official names for an expansive collection of mountain ranges that comprises much of the northern half of the Canadian province of British Columbia and a large area of southern Yukon.
The Northern Oregon Coast Range is the northern section of the Oregon Coast Range, in the Pacific Coast Ranges physiographic region, located in the northwest portion of the state of Oregon, United States. This section of the mountain range, part of the Pacific Coast Ranges, contains peaks as high as 3,710 feet (1,131 m) for Rogers Peak. Forests in these mountains are considered to be some of the most productive timber land in the world. The Central Oregon Coast Range is directly south of this section with the Southern Oregon Coast Range beyond the central range.
South Mountain is a Canadian range on the mainland portion of Nova Scotia. A granitic ridge stretching from the Annapolis Basin to Mount Uniacke, it forms the southern edge of the Annapolis Valley and shelters the valley from the climate effects of the pelagic coast along the Atlantic Ocean. Together with North Mountain, the two ranges form the Annapolis Highlands region.
Mount Nonotuck, 827 feet (252 m), is the northernmost peak of the Mount Tom Range of traprock mountains located in the Connecticut River Valley of Massachusetts and part of the larger Metacomet Ridge which stretches from Long Island Sound to nearly the Vermont border. Rugged and considered scenic, the peak rises steeply from the river valley 700 feet (210 m) below. It is located within the town of Holyoke.
The Laurentian Upland is a physiographic region which, when referred to as the "Laurentian Region" or the Grenville geological province, is recognized by Natural Resources Canada as one of five provinces of the larger Canadian Shield physiographic division. The United States Geological Survey recognizes the Laurentian Upland as the larger general upland area of the Canadian Shield.
The Hogem Ranges are a group of mountain ranges in the northwest part of the Omineca Country of the North-Central Interior of British Columbia, Canada, located between Takla Lake (W) and the Omineca River (E) and from the Nation Lakes (SE) to the Sustut River (NW). The ranges have a collective area of 8868 km2 and is a subgrouping of the Omineca Mountains which in turn form part of the Interior Mountains.
The Bulkley Ranges are a mountain range in northern British Columbia, Canada, located between the Skeena and Bulkley Rivers south of Hazelton, north of the Morice River and Zymoetz River. It has an area of 7851 km2 and is a subrange of the Hazelton Mountains which in turn form part of the Interior Mountains.
The Nikanassin Formation is a stratigraphic unit of Late Jurassic (Portlandian) to Early Cretaceous (Barremian) age. It is present along the western edge of the Western Canada Sedimentary Basin in western Alberta and northeastern British Columbia. Its name was first proposed by D.B. Dowling in 1909 (Coal Fields South of Grand Trunk Pacific Railway, in the foothills of the Rocky Mountain, Alberta Page 140 paragraph 4 " to this it is proposed to give the name Nikanassin, from the Cree word meaning outer range" Also it is noted on the map by D.B. Dowling.(Geological Survey of Canada. Incorrect info follows: It was named by B.R. MacKay in 1929 for the Nikanassin Range of the front-central ranges of the Canadian Rockies. Mackay did not designate a type locality for the formation, although he described outcrops near the hamlet of Brûlé, north of the Yellowhead Highway outside of Jasper National Park.
The Babine Range is a small subrange of the Skeena Mountains of the Interior Mountains, located between Babine Lake, Babine River, Bulkey River and Skeena River in northern British Columbia, Canada.
The Lizard Range is a mountain range southwest of Fernie, British Columbia in the Canadian Rockies. The range is home to the Fernie Alpine Resort and parts of the Mount Fernie Provincial Park.
The Kootenay Group, originally called the Kootenay Formation, is a geologic unit of latest Jurassic to earliest Cretaceous age in the Western Canada Sedimentary Basin that is present in the southern and central Canadian Rockies and foothills. It includes economically important deposits of high-rank bituminous and semi-anthracite coal, as well as plant fossils and dinosaur trackways.
 | This article related to a mountain, mountain range, or peak in British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |
 | This article about a location in the Interior of British Columbia, Canada is a stub. You can help Wikipedia by expanding it. |
