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Salmon Inlet
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 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 long; Clowhom Lake, covering a waterfall on the Clowhom River, stretches a further 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 An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to semiarid climates, but a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trips 05 - Sechelt Inlet - 11 (90968058)
The Agreement on Trade-Related Aspects of Intellectual Property Rights (TRIPS) is an international agreement, international legal agreement between all the member nations of the World Trade Organization (WTO). It establishes minimum standards for the regulation by national governments of different forms of intellectual property (IP) as applied to nationals of other WTO member nations. TRIPS was negotiated at the end of the Uruguay Round of the General Agreement on Tariffs and Trade (GATT) between 1989 and 1990 and is administered by the WTO. The TRIPS agreement introduced intellectual property law into the multilateral trading system for the first time and remains the most comprehensive multilateral agreement on intellectual property to date. In 2001, developing countries, concerned that developed countries were insisting on an overly narrow reading of TRIPS, initiated a round of talks that resulted in the Doha Declaration. The Doha declaration is a WTO statement that clarifies ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cheakamus Canyon
{{disambiguation, geo ...
Cheakamus is an anglicization of Chiyakmesh, the Skwxw7mesh language name for one of their villages, now located on Cheakamus Indian Reserve No. 11. Cheakamus may also refer to: *Cheakamus River *Cheakamus Lake *Cheakamus Powerhouse, on the Squamish River * ''Cheakamus'' (ship), see Union Steamship Company of British Columbia The Union Steamship Company of British Columbia was a pioneer firm on coastal British Columbia. It was founded in November 1889 by John Darling, a director of the Union Steamship Company of New Zealand, and nine local businessmen. The company beg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fjords Of British Columbia
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords whe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sechelt Inlets Marine Provincial Park
Sechelt Inlets Marine Provincial Park is a provincial park in British Columbia, Canada, at various locations on Sechelt Inlet, Salmon Inlet and Narrows Inlet, near Sechelt (Salmon Inlet and Narrows Inlet are side arms of Sechelt Inlet). Established initially as a recreation area in 1980, it was converted to a park in 1999, containing approximately . Individual sites within the park are: *Halfway Beach site, W side Sechelt Inlet *Thornhill Creek site; S side Salmon Inlet *Kunechin Point site, junction of Sechelt and Salmon Inlets, on N side *Tzoonie Narrows site, Narrows Inlet *Piper Point site, W side Sechelt Inlet *Skaiakos Point site, W side Sechelt Inlet See also *Mount Richardson Provincial Park *Skookumchuck Narrows Provincial Park *List of British Columbia provincial parks The British Columbia Parks and Protected Areas System is the collection of physical properties owned or administered by BC Parks, an agency of the British Columbia Ministry of Environment an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where flow emerges from a confined channel and is free to spread out and infiltrate the surface. This reduces the carrying capacity of the flow and results in deposition of sediments. The flow can take the form of infrequent debris flows or one or more ephemeral or perennial streams. Alluvial fans are common in the geologic record, such as in the Triassic basins of eastern North America and the New Red Sandstone of south Devon. Such fan deposits likely contain the largest accumulations of gravel in the geologic record. Alluvial fans have also been found on Mars ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mill (grinding)
A mill is a device, often a structure, machine or kitchen appliance, that breaks solid materials into smaller pieces by grinding, crushing, or cutting. Such comminution is an important unit operation in many processes. There are many different types of mills and many types of materials processed in them. Historically mills were powered by hand or by animals (e.g., via a hand crank), working animal (e.g., horse mill), wind (windmill) or water (watermill). In modern era, they are usually powered by electricity. The grinding of solid materials occurs through mechanical forces that break up the structure by overcoming the interior bonding forces. After the grinding the state of the solid is changed: the grain size, the grain size disposition and the grain shape. Milling also refers to the process of breaking down, separating, sizing, or classifying aggregate material (e.g. mining ore). For instance rock crushing or grinding to produce uniform aggregate size for construction purp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Logging
Logging is the process of cutting, processing, and moving trees to a location for transport. It may include skidding, on-site processing, and loading of trees or logs onto trucks or skeleton cars. Logging is the beginning of a supply chain that provides raw material for many products societies worldwide use for housing, construction, energy, and consumer paper products. Logging systems are also used to manage forests, reduce the risk of wildfires, and restore ecosystem functions, though their efficiency for these purposes has been challenged. In forestry, the term logging is sometimes used narrowly to describe the logistics of moving wood from the stump to somewhere outside the forest, usually a sawmill or a lumber yard. In common usage, however, the term may cover a range of forestry or silviculture activities. Illegal logging refers to the harvesting, transportation, purchase, or sale of timber in violation of laws. The harvesting procedure itself may be illegal, includin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Columbia Highway 99
Highway 99 is a provincial highway in British Columbia that serves Greater Vancouver and the Squamish–Lillooet corridor over a length of . It is a major north–south artery within Vancouver and connects the city to several suburbs as well as the U.S. border, where it continues south as Interstate 5. The central section of the route, also known as the Sea to Sky Highway, serves the communities of Squamish, Whistler, and Pemberton. Highway 99 continues through Lillooet and ends at a junction with Highway 97 near Cache Creek. The highway's number, assigned in 1940, was derived from former U.S. Route 99, the predecessor to Interstate 5 and a major route for the U.S. West Coast. Highway 99 originally comprised the King George Highway in Surrey, portions of Kingsway from New Westminster to Vancouver, and local streets. It was extended across the Lions Gate Bridge and to Horseshoe Bay in the 1950s along a new highway that would later be incorporated into Highway 1 (the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Tantalus
Mount Tantalus is a mountain in southwestern British Columbia, Canada, located southeast of Falk Lake and south of Monmouth Mountain. It is the highest mountain in the Tantalus Range of the Pacific Ranges and is famous for its snow-covered face. Climate Based on the Köppen climate classification, Mount Tantalus is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall. As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. See also * Mount Dione * Geography of British Columbia * Geology of British Columbia The geology of British Columbia is a function of its location on th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clowhom Lake
Clowhom Lake is a reservoir in the Sechelt Inlet Sechelt Inlet formerly ''Seechelt Inlet'' is one of the principal inlets of the British Columbia Coast. The inlet is significant in that it almost makes an island of what is instead the Sechelt Peninsula, whose isthmus is at the town of Sechelt ... basin, located on the Clowhom River at the upper end of Salmon Inlet, the southern side-inlet of Sechelt Inlet. Formed by Clowhom Dam, the reservoir was formerly two lakes, Upper Clowhom Lake and Lower Clowhom Lake, and had been referred to prior to their merger from inundation as the Clowhom Lakes. References * *https://www.lakepedia.com/lake/clowhom-bc.html External linksaerial image of Clowhom dam and powerhouse, BC Hydro website [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clowhom River
The Clowhom River is a short, river in British Columbia. It flows into the head of the Salmon Inlet about 26.2 km west of Squamish. Course The Clowhom originates at the outlet of a tiny, unnamed lake on the south slopes of Mount Jimmy Jimmy. It flows south from there for about 4.4 km until it enters remote Phantom Lake. The river turns east upon exiting Phantom Lake and very soon drops over tall Phantom Falls, which is rumored to stand at least 500 feet high. From Phantom Falls, the river runs east for about 4.4 km before turning south for about 5.7 miles and then southwest for about 5 km before entering the north end of Clowhom Lake. The river flows through a dam upon exiting the south end of Clowhom Lake. It only flows about 0.3 km from the lake outlet as it soon reaches its mouth in the Salmon Inlet. Clowhom Dam The dam has a 21.0 meter high crest with an elevation of 55 meters above sea level, it was built in 1953 to provide 33MW of pow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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