Mount Bigelow (Washington) - Misplaced Pages

Mountain in Washington, United States

Mount Bigelow
East aspect, summit in upper right
Highest point
Elevation	8,449 ft (2,575 m)
Prominence	800 ft (244 m)
Parent peak	Raven Ridge (8,572 ft)
Isolation	1.71 mi (2.75 km)
Coordinates	48°13′05″N 120°21′15″W / 48.2180825°N 120.3540503°W / 48.2180825; -120.3540503
Naming
Etymology	Frank Ezra Bigelow
Geography
Mount BigelowLocation in WashingtonShow map of Washington (state)Mount BigelowMount Bigelow (the United States)Show map of the United States

Interactive map of
Country	United States
State	Washington
County	Chelan / Okanogan
Protected area	Lake Chelan-Sawtooth Wilderness
Parent range	Methow Mountains North Cascades Cascade Range
Topo map	USGS Martin Peak
Geology
Rock age	Eocene to Late Cretaceous
Rock type	Tonalitic Orthogneiss
Climbing
Easiest route	class 3 scrambling

Mount Bigelow is an 8,449-foot-elevation (2,575-meter) mountain summit located on the border shared by Okanogan and Chelan counties in Washington state.

Description

Mount Bigelow is set on the boundary of the Lake Chelan-Sawtooth Wilderness, on land managed by the Okanogan–Wenatchee National Forest. The peak is the southernmost point in the wilderness. Bigelow ranks as the fifth-highest peak on Sawtooth Ridge, 10th-highest peak in the Methow Mountains, and the 67th-highest in Washington. Other peaks of Sawtooth Ridge include Oval Peak, Star Peak, Hoodoo Peak, Courtney Peak, Switchback Peak, Martin Peak, and Raven Ridge which is the nearest higher neighbor, 1.69 miles (2.72 km) to the northeast of Bigelow. Precipitation runoff from the north side of the mountain drains into East Fork Buttermilk Creek en route to the Twisp River, the west slope drains to Lake Chelan via Prince Creek, and the east side of the mountain drains into tributaries of the Methow River. Topographic relief is significant as the summit rises over 1,300 feet (396 meters) above Upper Eagle Lake in 0.35 mile (0.56 km). This mountain's toponym was officially adopted in 1971 by the U.S. Board on Geographic Names. The mountain is named in memory of Frank E. Bigelow (1877–1969), an early homesteader in the Lake Chelan area who worked on trails for the Forest Service for many years.

Climate

Lying east of the Cascade crest, the area around Mount Bigelow is a bit drier than areas to the west. Summers can bring warm temperatures and occasional thunderstorms. Most weather fronts originate in the Pacific Ocean, and travel northeast toward the Cascade Mountains. As fronts approach the North Cascades, they are forced upward by the peaks (orographic lift), causing them to drop their moisture in the form of rain or snowfall onto the Cascades. As a result, the North Cascades experience 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.

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 sections of the river valleys are 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.