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The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as many of those in the North Cascades, and the notable volcanoes known as the High Cascades.
The North Cascades are a section of the Cascade Range of western North America. They span the border between the Canadian province of British Columbia and the U.S. state of Washington and are officially named in the U.S. and Canada [ 1 ] as the Cascade Mountains . [ 2 ]
The Cascades, a terminus of the Los Angeles Aqueduct, US; Cascades, Isle of Dogs, a building in London, England; Cascades FC, a Tasmanian soccer club from 1931 to 1936; Cascades Female Factory, a former Australian workhouse for female convicts in Hobart, Tasmania; Oregon State University Cascades Campus, a branch campus in Bend, Oregon, US
North Cascades National Park is a national park of the United States in Washington.At more than 500,000 acres (200,000 ha), it is the largest of the three National Park Service units that comprise the North Cascades National Park Complex.
Mount Shasta (northern California) — second highest peak in the Cascades. Can be seen in the Sacramento Valley as far as 140 mi (230 km) away, as it is a dominating feature of the region. Lassen Peak (south of Mount Shasta) — southernmost volcano in the Cascades and the most easily climbed peak in the Cascades. It erupted from 1914 to 1921 ...
Forecast models show more than 6 inches of rainfall could occur in the highest rainfall accumulation zones, while feet of snow look likely from the extreme northern Sierra Nevada into the Cascades.
The geography of the North Cascades describes a range of rugged mountains in British Columbia, Canada and Washington, United States. In Canada, the range is officially named the Cascade Mountains but is commonly referred to as the Canadian Cascades.
The West Cascades period came to an end 17 million years ago when the Columbia River flood basalts began erupting in eastern Washington and Oregon. [2] For a reason unknown to scientists the initiation of the flood basalts seemingly caused a significant dip in volcanic activity in the cascade chain lasting for over 8 million years. [2]