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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 often referred as the "American Alps" by hikers, climbers and mountaineers because of the sea of steep, jagged peaks that span across the range. This range's rugged approaches and exceptional alpine terrain make it a premiere training ground for mountain climbers.
As fronts approach the North Cascades, they are forced upward by the peaks of the Cascade Range (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. [7]
The Enchantments is a region within the Alpine Lakes Wilderness area of Washington state's Cascade Mountain Range. [2] At an elevation of 4,500 feet (1,372 m), it is home to over 700 alpine lakes and ponds surrounded by the vast peaks of Cashmere Crags, which rate among the best rock-climbing sites in the western United States. [3]
The Triad is a mountain with three peaks located in the North Cascades, in Skagit County of Washington state. [5] Situated in North Cascades National Park, The Triad is positioned west of the crest of the Cascade Range, approximately 12 miles east of the town of Marblemount.
The summit is situated about 4 miles (6.4 km) east of the Mountain Loop Highway. Sloan Peak has been called the "Matterhorn of the Cascades" for its sharp, high peak, which is accentuated by its impressive local relief and its isolated position west of the Cascade crest. It is easily visible from many locations in the North Cascades.
Mount Index is a peak in the central part of the Cascade Range of Washington state. It lies just south of the Skykomish River and U.S. Route 2, at the western edge of the Cascades. Despite its low elevation relative to peaks higher in the Cascades, it is a famous and dramatic landmark due to its topographic prominence. It comprises three ...
The Cascade Mountains form the northern portion of the Cascade-Sierra province. The Cascades were created from thousands of small, short-lived volcanoes along the Cascadia subduction zone [ 5 ] that over millions of years built a foundation of lava and volcanic debris on which the mountains rise.