Big Four Mountain

History

Big Four is not named for the five peaks on its top. Possible origins for its name include a figure four that is visible in one of its snowfields and a group of four brothers who were known to prospect and trap in the valley. The snow accumulation at the location of the ice caves was known as "Rucker's Glacier" (not actually a glacier), and is considered the lowest elevation permanent ice in the Cascades.

Big Four Inn was a resort near the base of the mountain built by the Rucker Brothers in 1921 until it was destroyed by fire in 1949.{{Historylink

The first ascent of Big Four was made July 19, 1931, by Forest Farr and Art Winder via the northwest ridge.

Climate

Big Four Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and 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 snowfall 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. 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. Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. The months July through September offer the most favorable weather for viewing or climbing this peak.

Geology

The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, ridges, and deep glacial valleys. Geological events occurring many years ago created the diverse topography and drastic elevation changes over the Cascade Range leading to the various climate differences. These climate differences lead to vegetation variety defining the ecoregions in this area.

The history of the formation of the Cascade Mountains dates back millions of years ago to the late Eocene Epoch. With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.

During the Pleistocene period dating back over two million years ago, glaciation advancing and retreating repeatedly scoured the landscape leaving deposits of rock debris. The U-shaped cross section of the river valleys is a result of 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 North Cascades area.

Gallery

File:Big Four Mountain.jpg|Big Four Mountain viewed from Dickerman Mountain File:Big Four Mountain WA.jpg| File:Big Four Mountain with Big Four Inn and cabins, Snohomish County, Washington, ca 1923 (WASTATE 1265).jpeg|Big Four Mountain with Hall Peak to right, Big Four Inn in lower right. ca 1923 File:Big Four Glacier Ice cave.jpg|One of Big Four's ice caves, ca. 1920. File:Exterior of Big Four Inn with rail car, near Monte Cristo, Snohomish County, Washington, ca 1923 (WASTATE 674).jpeg|Big Four Inn and mountain File:Big Four Inn, Big Four Mountain and cabins near Monte Cristo, Snohomish County, Washington, ca 1923 (WASTATE 1266).jpeg|Pemmican Peak, Big Four Inn and cabins File:Big Four Inn lobby, Snohomish County, Washington, ca 1923 (WASTATE 1268).jpeg|Big Four Inn lobby

References

References

1. {{cite peakbagger
2. "Big Four Mountain - 6,180' WA".
3. {{cite gnis
4. (August 2, 2010). "Girl killed by falling ice at Big Four Ice Caves identified". The Seattle Times.
5. (July 7, 2015). "One Killed, Four Injured as Washington State Ice Caves Collapse Again". NBC News.
6. "History of Darrington > Origin Of Area Names > Big Four Mountain".
7. Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
8. Kruckeberg, Arthur. (1991). "The Natural History of Puget Sound Country". University of Washington Press.