The Continental Divide of the Americas is the principal, and largely mountainous, hydrological divide of the Americas. The Continental Divide extends from the Bering Strait to the Strait of Magellan, and separates the watersheds that drain into the Pacific Ocean from those river systems that drain into the Atlantic and Arctic Ocean, including those that drain into the Gulf of Mexico, the Caribbean Sea, and Hudson Bay.
The Skeena River is the second-longest river entirely within British Columbia, Canada. Since ancient times, the Skeena has been an important transportation artery, particularly for the Tsimshian and the Gitxsan—whose names mean "inside the River of Mist" ,and "people of the River of Mist," respectively. The river and its basin sustain a wide variety of fish, wildlife, and vegetation, and communities native to the area depend on the health of the river. The Tsimshian migrated to the Lower Skeena River, and the Gitxsan occupy territory of the Upper Skeena.
Burrard Inlet is a shallow-sided fjord in the northwestern Lower Mainland, British Columbia, Canada. Formed during the last Ice Age, it separates the City of Vancouver and the rest of the lowland Burrard Peninsula to the south from the coastal slopes of the North Shore Mountains, which span West Vancouver and the City and District of North Vancouver to the north.
Shuswap Lake is a lake located in the southern interior of British Columbia, Canada that drains via the Little Shuswap River into Little Shuswap Lake. Little Shuswap Lake is the source of the South Thompson River, a branch of the Thompson River, a tributary of the Fraser River. It is at the heart of a region known as the Columbia Shuswap or "the Shuswap", noted for its recreational lakeshore communities including the city of Salmon Arm. The name "Shuswap" is derived from the Shuswap or Secwepemc First Nations people, the most northern of the Interior Salish peoples, whose territory includes the Shuswap. The Shuswap call themselves /ʃǝxwépmǝx/ in their own language, which is called /ʃǝxwepmǝxtʃín/.
Triple Divide Peak is located in the Lewis Range, part of the Rocky Mountains in North America. The peak is a feature of Glacier National Park in the state of Montana in the United States. The summit of the peak, the hydrological apex of the North American continent, is the point where two of the principal continental divides in North America converge, the Continental Divide of the Americas and the Northern or Laurentian Divide.
The Mount Meager massif is a group of volcanic peaks in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. Part of the Cascade Volcanic Arc of western North America, it is located 150 km (93 mi) north of Vancouver at the northern end of the Pemberton Valley and reaches a maximum elevation of 2,680 m (8,790 ft). The massif is capped by several eroded volcanic edifices, including lava domes, volcanic plugs and overlapping piles of lava flows; these form at least six major summits including Mount Meager which is the second highest of the massif.
Mount Price is a small stratovolcano in the Garibaldi Ranges of the Pacific Ranges in southwestern British Columbia, Canada. It has an elevation of 2,049 metres and rises above the surrounding landscape on the western side of Garibaldi Lake in New Westminster Land District. The mountain contains a number of subfeatures, including Clinker Peak on its western flank, which was the source of two thick lava flows between 15,000 and 8,000 years ago that ponded against glacial ice. These lava flows are structurally unstable, having produced large landslides as recently as the 1850s. A large provincial park surrounds Mount Price and other volcanoes in its vicinity. It lies within an ecological region that surrounds much of the Pacific Ranges.
Loss Creek is a river in the Capital Regional District of British Columbia, Canada. Located on southern Vancouver Island, it flows through a long, steep-sided valley to the Strait of Juan de Fuca on the Pacific Ocean.
Maitland Volcano is a heavily eroded shield volcano in the Northern Interior of British Columbia, Canada. It is 83 km (52 mi) southeast of the small community of Telegraph Creek in what is now the Klappan Range of the northern Skeena Mountains. This multi-vent volcano covered a remarkably large area and was topped by a younger volcanic edifice. Little remains of Maitland Volcano today, limited only to eroded lava flows and distinctive upstanding landforms created when magma hardened within the vents of the volcano.
Salmon Inlet, formerly Salmon Arm, is a fjord branching east from Sechelt Inlet in the British Columbia, Canada. Its companion, Narrows Inlet, another side-inlet of Sechelt Inlet, lies roughly 10 km (6.2 mi) north. Misery and Sechelt Creeks flow freely into the inlet, while the Clowhom River flows in from the artificial Clowhom Lake, formed by a small hydroelectric power development. The fjord is 23 km (14 mi) long; Clowhom Lake, covering a waterfall on the Clowhom River, stretches a further 12 km (7.5 mi) to the western base of Mount Tantalus, which is best known from the direction of Squamish and the Cheakamus Canyon stretch of British Columbia Highway 99. Heavily affected by logging and milling operations, the inlet is split almost into two portions by an alluvial fan spreading from the mouth of Sechelt Creek.
The Indian River is a river in Yukon, Canada. It is in the Bering Sea drainage basin and is a right tributary of the Yukon River.
Scum Lake is a lake in the Chilcotin region of the Interior of British Columbia, Canada.
Nanaimo River is a river on Vancouver Island, British Columbia, Canada, located near the city of Nanaimo on the island's east coast. Its headwaters are in the Vancouver Island Ranges of central Vancouver Island and its mouth, the Nanaimo River estuary, is at the south end of Nanaimo Harbour in the Strait of Georgia. The estuary is part of the Pacific Estuary Conservation Program.
A triple divide or triple watershed is a point on Earth's surface where three drainage basins meet. A triple divide results from the intersection of two drainage divides. Triple divides range from prominent mountain peaks to minor side peaks, down to simple slope changes on a ridge which are otherwise unremarkable. The elevation of a triple divide can be thousands of meters to barely above sea level. Triple divides are a common hydrographic feature of any terrain that has rivers, streams and/or lakes.
Percy Creek is a stream in the southeastern part of the District of North Vancouver in the Lower Mainland part of British Columbia, Canada. It is in the Pacific Ocean drainage basin and is a right tributary of Indian Arm.
Moonbeam Creek is a stream in Thompson-Nicola Regional District in the Interior region of British Columbia, Canada. It is in the Pacific Ocean drainage basin and is a left tributary of the North Thompson River. The nearest communities to the mouth of the creek on British Columbia Highway 5 are Blue River 40 kilometres (25 mi) south and Valemount 50 kilometres (31 mi) north; the mouth of the creek is just downstream of confluence of the North Thompson River and the Albreda River, where the North Thompson River turns 90° right and heads south.
The Albreda River is a river in Thompson-Nicola Regional District and the Regional District of Fraser-Fort George in the Interior region of British Columbia, Canada. It is in the Pacific Ocean drainage basin and is a left tributary of the North Thompson River. The nearest communities to the mouth of the creek on British Columbia Highway 5 are Blue River 42 kilometres (26 mi) south and Valemount 48 kilometres (30 mi) north; the mouth of the river is at a point where the North Thompson River, arriving downstream from its source, turns 90° right and heads south.
Canvas Creek is a stream in Kamloops Division Yale Land District in the Interior region of British Columbia, Canada. It is in the Pacific Ocean drainage basin and is a right tributary of the North Thompson River.
Noyse Creek is a river in the Capital Regional District of British Columbia, Canada. Located on southern Vancouver Island, it flows from its source to its mouth as a right tributary of Loss Creek. The upper reaches of the creek were originally logged in 1967-1975 and replanted. The surrounding forest is now a prime example of a 50-year old second growth eco-system.
Gain Creek is a river in the Capital Regional District of British Columbia, Canada. Located on southern Vancouver Island, it flows from its source to its mouth as a right tributary of Loss Creek.
