Big Snow Mountain
Mountain summit of the Cascade Range in King County, Washington State From Wikipedia, the free encyclopedia
Big Snow Mountain is a prominent 6,680-foot (2,040-metre) mountain summit located 7 mi (11 km) north of Snoqualmie Pass in the Alpine Lakes Wilderness in eastern King County of Washington state.[4] It is part of the Cascade Range and is situated on land managed by Mount Baker-Snoqualmie National Forest. Precipitation runoff from the mountain drains into tributaries of the Snoqualmie and Skykomish Rivers. The nearest higher peak is Overcoat Peak, 3.75 mi (6.04 km) to the east-southeast.[1]
| Big Snow Mountain | |
|---|---|
 Big Snow Mountain from Snoqualmie Mountain | |
| Highest point | |
| Elevation | 6,680 ft (2,036 m)[1] |
| Prominence | 1,360 ft (415 m)[1] |
| Parent peak | Overcoat Peak (7,432 ft)[2] |
| Isolation | 3.74 mi (6.02 km)[2] |
| Coordinates | 47°32′06″N 121°21′58″W[1] |
| Geography | |
  Big Snow Mountain Location in Washington  Big Snow Mountain Location in the United States | |
| Country | United States |
| State | Washington |
| County | King |
| Protected area | Alpine Lakes Wilderness |
| Parent range | Cascade Range |
| Topo map | USGS Big Snow Mountain |
| Geology | |
| Type of rock | Keechelus andesite |
| Climbing | |
| First ascent | 1917 by The Mountaineers[3] |
| Easiest route | Scrambling |
Big Snow Mountain is located in the marine west coast climate zone of western North America.[3] Weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains. As fronts approach, they are forced upward by the peaks of the Cascade Range, causing them to drop their moisture in the form of rain or snow onto the Cascades (Orographic lift). As a result, the west side of the Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger.[3] During winter months, weather is usually cloudy, but, due to high pressure systems over the Pacific Ocean that intensify during summer months, there is often little or no cloud cover during the summer.[3]
The Alpine Lakes Wilderness features some of the most rugged topography in the Cascade Range with craggy peaks and ridges, deep glacial valleys, and granite walls spotted with over 700 mountain lakes.[5] Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences.
The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch.[6] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted.[6] In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.[6]
During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured and shaped the landscape.[6] The last glacial retreat in the Alpine Lakes area began about 14,000 years ago and was north of the Canada–US border by 10,000 years ago.[6] The U-shaped cross section of the river valleys is a result of that recent glaciation. Uplift and faulting in combination with glaciation have been the dominant processes which have created the tall peaks and deep valleys of the Alpine Lakes Wilderness area.
Southwest aspect, from Mount Defiance
East aspect
Big Snow summit detail
Big Snow Mountain summit panorama showing Summit Chief Mountain, Chimney Rock, and Lemah
Wikiwand in your browser!
Seamless Wikipedia browsing. On steroids.
Every time you click a link to Wikipedia, Wiktionary or Wikiquote in your browser's search results, it will show the modern Wikiwand interface.
Wikiwand extension is a five stars, simple, with minimum permission required to keep your browsing private, safe and transparent.
