Similkameen Falls
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Similkameen Falls
Similkameen Falls is a waterfall in British Columbia, Canada, on the Similkameen River located just below the mouth of the Pasayten River and just above the mouth of Copper Creek about 25 km upstream (south) from Princeton. The name ''Similkameen Falls'' is a rarely used alternate name for Coyote Falls, which is located further downstream in the US state of Washington so sometimes this one is confused with Coyote. Stature Similkameen Falls actually resembles a major series of rapids more than a waterfall. Over a stretch of about 0.2 km, the river drops about 25 feet at the bottom of a canyon. Huge walls of igneous rock, some about 250 feet high, rise above the falls on both sides. The first drop of the falls is a small but powerful chute. No more than 3 feet wide, the entire river is forced through it, so it is fairly powerful. At the end of the chute, the river plunges powerfully into a deep pool in a punchbowl form. Remains of an old bridge that used to cross t ...
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Princeton, British Columbia
Princeton (originally Vermilion Forks) is a town in the Similkameen region of southern British Columbia, Canada."The rich history of Princeton or how Vermilion Forks made it on the map...", Princeton 2008 Visitors Guide, p. 4. It lies just east of the Cascade Mountains, which continue south into Washington, Oregon and California. The Tulameen and Similkameen Rivers converge here."Everything you've ever wanted to know about Princeton...", Princeton 2008 Visitors Guide, p. 6. At the 2016 census, the population was 2,828. Princeton centres on seven blocks of businesses along Bridge Street and five blocks on Vermilion Avenue; there are also businesses along British Columbia Highway 3."Princeton... 'Beautiful B.C. at its Best'", Princeton 2008 Visitors Guide, p. 9. Historically, the area's main industry has been mining—copper, gold, coal, and some platinum—The town's biggest employers are Copper Mountain Mine and a sawmill owned by Weyerhaeuser, along with a few smaller timbe ...
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Similkameen River
The Similkameen River runs through southern British Columbia, Canada, eventually discharging into the Okanagan River near Oroville, Washington, in the United States. Through the Okanagan River, it drains to the Columbia River. The river is said to be named for an indigenous people called ''Similkameigh'', meaning "treacherous waters". The river is controversially dammed (the now-defunct Enloe Dam), blocking fish passage to the upper (Canadian) reaches of the river. History The first mention of the Similkameen by a European was by Alexander Ross. While on a trading expedition, he travelled by way of the "Similkameigh River." Sir George Simpson used the name "Similkameigh" for one of the groups part of the Okanagan Nation. The transition from ''Similkameigh'' to ''Similkameen'' may have been inspired by the name of the Tulameen River despite being etymologically incorrect. The name ''Similkameigh'' comes from a now-extinct language of Nicola-Similkameen, of the Athapascan lan ...
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Waterfall
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is general ...
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British Columbia
British Columbia (commonly abbreviated as BC) is the westernmost Provinces and territories of Canada, province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, forests, lakes, mountains, inland deserts and grassy plains, and borders the province of Alberta to the east and the Yukon and Northwest Territories to the north. With an estimated population of 5.3million as of 2022, it is Canada's Population of Canada by province and territory, third-most populous province. The capital of British Columbia is Victoria, British Columbia, Victoria and its largest city is Vancouver. Vancouver is List of census metropolitan areas and agglomerations in Canada, the third-largest metropolitan area in Canada; the 2021 Canadian census, 2021 census recorded 2.6million people in Metro Vancouver Regional District, Metro Vancouver. The First Nations in Canada, first known human inhabi ...
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Pasayten River
The Pasayten River is a tributary of the Similkameen River, in the Canadian province of British Columbia and the U.S. state of Washington. The Pasayten River is part of the Columbia River drainage basin, being a tributary of the Similkameen River, which flows into the Okanagan River, which flows into the Columbia River. Course The Pasayten River originates in the North Cascades part of the Cascade Range. It flows generally north through the Pasayten Wilderness and across the international boundary. West Fork The West Fork Pasayten River originates on the north slopes of Slate Peak and flows north until it reaches Three Forks, where it and the Middle Fork converge to form the Pasayten River Proper. Rock Creek also joins here, which makes the name "Three Forks" very appealing to not only the three way confluence, but to the nearby cabin. Middle Fork The Middle Fork Pasayten River originates in Slate Pass and flows north until it reaches Three Forks, where it and the West F ...
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Copper Creek (British Columbia)
Copper Creek can refer to several streams: *Copper Creek (Valdez-Cordova Borough, Alaska) (several with that name) *Copper Creek (Denali Borough, Alaska) *Copper Creek (California) *Copper Creek (Washington) Copper Creek can refer to several streams: *Copper Creek (Valdez-Cordova Borough, Alaska) (several with that name) *Copper Creek (Denali Borough, Alaska) *Copper Creek (California) Copper Creek (also called the Copper River, natively called Chw ... * Copper Creek (Wisconsin), a stream in Sauk County {{disambig ...
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Washington (state)
Washington (), officially the State of Washington, is a state in the Pacific Northwest region of the Western United States. Named for George Washington—the first U.S. president—the state was formed from the western part of the Washington Territory, which was ceded by the British Empire in 1846, by the Oregon Treaty in the settlement of the Oregon boundary dispute. The state is bordered on the west by the Pacific Ocean, Oregon to the south, Idaho to the east, and the Canadian province of British Columbia to the north. It was admitted to the Union as the 42nd state in 1889. Olympia is the state capital; the state's largest city is Seattle. Washington is often referred to as Washington state to distinguish it from the nation's capital, Washington, D.C. Washington is the 18th-largest state, with an area of , and the 13th-most populous state, with more than 7.7 million people. The majority of Washington's residents live in the Seattle metropolitan area, the center o ...
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Rapids
Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Rapids are hydrological features between a ''run'' (a smoothly flowing part of a stream) and a ''cascade''. Rapids are characterized by the river becoming shallower with some rocks exposed above the flow surface. As flowing water splashes over and around the rocks, air bubbles become mixed in with it and portions of the surface acquire a white color, forming what is called "whitewater". Rapids occur where the bed material is highly resistant to the erosive power of the stream in comparison with the bed downstream of the rapids. Very young streams flowing across solid rock may be rapids for much of their length. Rapids cause water aeration of the stream or river, resulting in better water quality. Rapids are categorized in classes, generally running from I to VI. A Class 5 rapid may be categorized as Class 5.1-5.9. While Class I rapids are ...
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Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type ...
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Igneous Rock
Igneous rock (derived from the Latin word ''ignis'' meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet's mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, or without crystallization to form natural glasses. Igneous rocks occur in a wide range of geological settings: shields, platforms, orogens, basins, large igneous provinces, extended crust and oceanic crust. Geological significance Igneous and metamorphic rocks make up 90–95% of the top ...
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Highway 3 From Similkameen Falls
A highway is any public or private road or other public way on land. It is used for major roads, but also includes other public roads and public tracks. In some areas of the United States, it is used as an equivalent term to controlled-access highway, or a translation for ''autobahn'', '' autoroute'', etc. According to Merriam Webster, the use of the term predates the 12th century. According to Etymonline, "high" is in the sense of "main". In North American and Australian English, major roads such as controlled-access highways or arterial roads are often state highways (Canada: provincial highways). Other roads may be designated "county highways" in the US and Ontario. These classifications refer to the level of government (state, provincial, county) that maintains the roadway. In British English, "highway" is primarily a legal term. Everyday use normally implies roads, while the legal use covers any route or path with a public right of access, including footpaths etc. The ...
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Crowsnest Highway
The Crowsnest Highway is an east-west highway in British Columbia and Alberta, Canada. It stretches across the southern portions of both provinces, from Hope, British Columbia to Medicine Hat, Alberta, providing the shortest highway connection between the Lower Mainland and southeast Alberta through the Canadian Rockies. Mostly two-lane, the highway was officially designated in 1932, mainly following a mid-19th-century gold rush trail originally traced out by an engineer named Edgar Dewdney. It takes its name from the Crowsnest Pass, the location at which the highway crosses the Continental Divide between British Columbia and Alberta. In British Columbia, the highway is entirely in mountainous regions and is also known as the Southern Trans-Provincial Highway. The first segment between the Trans-Canada Highway and Highway 5A is locally known as the Hope-Princeton Highway, and passes by the site of the Hope Slide. In Alberta, the terrain is initially mountainous, before smo ...
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