Foggy Peak | |
---|---|
Highest point | |
Elevation | 6,810 ft (2,076 m) [1] [2] |
Prominence | 750 ft (229 m) [3] |
Parent peak | Cadet Peak (7,186 ft) [3] |
Isolation | 1.16 mi (1.87 km) [3] |
Coordinates | 47°59′52″N121°21′57″W / 47.9978076°N 121.3659479°W [4] |
Geography | |
Country | United States |
State | Washington |
County | Snohomish |
Protected area | Henry M. Jackson Wilderness |
Parent range | Cascade Range |
Topo map | USGS Blanca Lake |
Climbing | |
First ascent | No record [1] |
Easiest route | class 4 scrambling [3] |
Foggy Peak is a 6,810-foot-elevation (2,076-meter) mountain summit in Snohomish County of Washington state.
Foggy Peak is located in the North Cascades four miles (6.4 km) southeast of Barlow Pass and immediately northeast of the historic Monte Cristo townsite. It is set within the Henry M. Jackson Wilderness on land administered by the Mount Baker-Snoqualmie National Forest. Precipitation runoff from the mountain drains into tributaries of the Sauk River. Topographic relief is significant as the summit rises 4,000 feet (1,200 meters) above Monte Cristo in 1.5 mile (2.4 km) and 3,650 feet (1,110 meters) above Goat Lake in 1.35 mile. Foggy Peak's nearest higher neighbor is Cadet Peak, 1.16 mi (1.87 km) to the southeast. [2] Back in the old mining days, the long sub-range stretching from Cadet Peak to Sheep Mountain was known as Pride of the Mountains Range. [1] Cadet Peak was originally called Foggy Peak, for the Foggy Mine claim on the mountain's north slope, but the name was changed in 1896 and the Foggy Peak name was transferred to its present location. [1] The peak's toponym was officially adopted by the U.S. Board on Geographic Names in 1918. [4] When the board adopted the name, it described a glacier on the peak's east slope, [5] however satellite imagery shows a mere snowfield remains.
Foggy Peak is located in the marine west coast climate zone of western North America. [1] Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains. 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. [1] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. [1] 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. [1] Due to its temperate climate and proximity to the Pacific Ocean, areas west of the Cascade Crest very rarely experience temperatures below 0 °F (−18 °C) or above 80 °F (27 °C). [1] The months July through September offer the most favorable weather for viewing or climbing this peak.
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. [6] With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. [6] Glacier Peak, a stratovolcano that is 14 mi (23 km) northeast of Foggy Peak, began forming in the mid-Pleistocene. [1] 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 the landscape leaving deposits of rock debris. [6] 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.
Monte Cristo Peak is a mountain peak in the Henry M. Jackson Wilderness in Washington state. Together with Columbia Peak and Kyes Peak it forms a basin that contains Columbia Glacier and Blanca Lake. The 1918 edition of The Mountaineer called the mountain "a huge pile of red rock."
Columbia Peak is a mountain peak in the Henry M. Jackson Wilderness in the U.S. state of Washington. Columbia Peak rises to 7,172 feet (2,186 m). Together with Monte Cristo Peak and Kyes Peak it forms a basin that contains Columbia Glacier and Blanca Lake.
Bacon Peak is a mountain located in North Cascades National Park, in the Cascade Range in the U.S. state of Washington. Its glaciers cover 1.2 square miles (3.2 km2); the three main glaciers are Diobsud Creek Glacier, Green Lake Glacier and Noisy Creek Glacier.
Stillaguamish Peak is a 5,720+ ft mountain summit near the western edge of the North Cascades, in Snohomish County of Washington state. It is located five miles north-northwest of Barlow Pass near the Monte Cristo area, and is situated on land administered by the Mount Baker-Snoqualmie National Forest. It rises 4,000 feet (1,200 m) above the Stillaguamish River and the Mountain Loop Highway.
Del Campo Peak is a prominent summit near the western edge of the North Cascades, in Snohomish County of Washington state. It is located south of Barlow Pass along the Mountain Loop Highway near the Monte Cristo area. It is situated on land administered by the Mount Baker-Snoqualmie National Forest. The mountain is named for a mining claim on the mountain's slope. The nearest peak is Gothic Peak, 0.5 miles (0.80 km) to the southwest, and Foggy Pass is the low point between the two peaks. Foggy Lake lies in Gothic Basin below the south face of Del Campo Peak and collects precipitation runoff which ultimately drains to South Fork Sauk River via Weden Creek. Runoff from the west side of the mountain drains into the Sultan River, and the north side drains into headwaters of the Stillaguamish River. In terms of favorable weather, the best months for climbing are July through September.
Sheep Mountain is a 6,166-foot-elevation (1,879-meter) summit near the western edge of the North Cascades, in Snohomish County of Washington state. It is located one mile east of Barlow Pass along the Mountain Loop Highway near the Monte Cristo area. It is situated on land administered by the Mount Baker-Snoqualmie National Forest. Back in the old mining days of the late 1800s, the long sub-range stretching from Cadet Peak to Sheep Mountain was known as Pride of the Mountains Range. Precipitation runoff from the mountain drains into tributaries of the Sauk River.
Snowking Mountain is a 7,433-foot (2,266-metre) summit located in Skagit County of Washington state. Situated within the Glacier Peak Wilderness, Snowking Mountain is positioned west of the crest of the North Cascades, approximately 18 miles northeast of the town of Darrington. It is set within the Glacier Peak Wilderness, on land managed by Mount Baker–Snoqualmie National Forest. Snowking has two subsidiary peaks, West Peak (7,425 ft), and Middle Peak (7,400 ft). A broad unnamed glacier known colloquially as Snowking Glacier rests on the north face. Downslope of that glacier are Snowking Lake, Found Lake, and Cyclone Lake. Mount Tommy Thompson is three miles to the northwest, and the nearest higher neighbor is Mount Misch, 5.75 miles (9.25 km) to the southeast. Precipitation runoff from Snowking Mountain drains into tributaries of the Skagit River.
Cadet Peak is a 7,186 ft mountain summit near the western edge of the North Cascades, in Snohomish County of Washington state. The peak is located southeast of Barlow Pass along the Mountain Loop Highway, and two miles east of the historic Monte Cristo area. It is situated within the Henry M. Jackson Wilderness, on land administered by the Mount Baker-Snoqualmie National Forest. The mountain was originally called Foggy Peak, for the Foggy Mine claim on the mountain's north slope, but the name was changed in 1896 to its present name, and the Foggy Peak name was transferred to the peak immediately northwest of Cadet. Back in the old mining days, the long sub-range stretching from Cadet Peak to Sheep Mountain was known as Pride of the Mountains Range. Cadet's nearest higher neighbor is Kyes Peak, 1.59 mi (2.56 km) to the south-southeast. Precipitation runoff from the mountain drains into tributaries of the Sauk River.
Kololo Peaks is an 8,200+ ft mountain located in the Glacier Peak Wilderness of the North Cascades in Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Wenatchee National Forest. The nearest higher peak is Glacier Peak, 3.29 mi (5.29 km) to the north. Precipitation runoff and meltwater from the White River Glacier on the southeast slope drains into White River. On the west slope, the White Chuck Glacier drains into the White Chuck River, and the Suiattle Glacier and Honeycomb Glacier on the north and east sides drain into the Suiattle River. Surrounded by these glaciers, Fred Beckey in his Cascade Alpine Guide describes the mountain as being almost a nunatak.
White Mountain is a 7,043-foot (2,147-metre) mountain located in the Glacier Peak Wilderness of the North Cascades in Washington state. The mountain is situated on the crest of the Cascade Range, on the shared border of Snohomish County and Chelan County, and also straddling the boundary between Mount Baker-Snoqualmie National Forest and Wenatchee National Forest. White Mountain is located 3.04 mi (4.89 km) to the west-southwest of Kololo Peaks, and immediately north of White Pass. The Pacific Crest Trail traverses the south slope of the peak. Precipitation runoff from the peak drains into the White River, White Chuck River, and Sauk River. The mountain's name was suggested by The Mountaineers, and officially adopted in 1918 by the United States Board on Geographic Names.
Spider Mountain is an 8,317-foot (2,535-metre) mountain summit located in the Glacier Peak Wilderness in western Chelan County of Washington state. It is part of the North Cascades, which is a subset of the Cascade Range. Meltwater from the Spider Glacier on the steep north face, and other surface runoff from the mountain drains into Flat Creek, which is a tributary of the Stehekin River. Topographic relief is significant as the summit rises 4,200 feet above West Fork Flat Creek in one mile (1.6 km). The nearest higher neighbor is Mount Formidable 1.5 miles (2.4 km) to the west. The Middle Cascade Glacier lies between these two mountains and the Ptarmigan Traverse passes between the two.
Johnson Mountain is a 6,721-foot (2,049-metre) mountain summit located in the Glacier Peak Wilderness of the North Cascades in Washington state. The mountain is situated in eastern Snohomish County, in the Mt. Baker-Snoqualmie National Forest. Its nearest higher peak is White Mountain, 3.3 mi (5.3 km) to the northeast, along with Indian Head Peak 3.38 mi (5.44 km) to the east. Precipitation runoff from the mountain drains into tributaries of the Sauk River. The mountain's name honors Mackinaw Johnson, a prospector who had a cabin in the vicinity.
Mount Forgotten is a 6,005-foot-elevation (1,830-meter) mountain summit near the western edge of the North Cascades, in Snohomish County of Washington state. It is located five miles north of Barlow Pass along the Mountain Loop Highway near the Monte Cristo area and is situated on land administered by the Mount Baker-Snoqualmie National Forest. The nearest higher peak is Mount Pugh, 4.22 mi (6.79 km) to the northeast. Precipitation runoff from the mountain drains into tributaries of the Sauk River.
Gothic Peak is a 6,213-foot (1,894-metre) multi-peak mountain summit located near the western edge of the North Cascades Range, in Snohomish County of Washington state. It is located south of Barlow Pass along the Mountain Loop Highway near the Monte Cristo area. It is situated on land administered by the Mount Baker-Snoqualmie National Forest. The mountain was named for early prospector William Gothic, who was one of the first to stake a claim in Gothic Basin. The mountain's name was officially adopted in 1967. The nearest higher peak is Del Campo Peak, 0.5 miles (0.80 km) to the northeast, and Foggy Pass is the low point between the two peaks. Foggy Lake lies in Gothic Basin below the east face of Gothic Peak and collects precipitation runoff which ultimately drains to South Fork Sauk River via Weden Creek. Runoff from the west side of the mountain drains into the Sultan River. The first ascent of the mountain was made on June 10, 1934, by Don Blair, Willard Carr, Norval Grigg, and Art Winder. In terms of catching favorable weather, the best months for climbing are July through September.
Riddle Peaks, also known as Riddle Peak, is an 8,212-foot (2,503-metre) mountain summit located at the head of Riddle Creek in the North Cascades, in Chelan County of Washington state. Riddle Peak is situated on the Glacier Peak Wilderness boundary, six miles west of Lake Chelan, and 2.5 mi (4.0 km) northeast of Holden, on land managed by the Wenatchee National Forest. The nearest higher neighbor is Flora Mountain, 2.25 miles (3.62 km) to the northeast, and Martin Peak lies 3.7 miles (6.0 km) to the west-northwest. Precipitation runoff from the mountain drains into Lake Chelan via Railroad Creek, Riddle Creek, and Devore Creek. Topographic relief is significant since the southern aspect of the mountain rises 5,000 feet above the Railroad Creek valley in approximately 2 mi (3.2 km). The first ascent of the peak was made September 11, 1940, by Everett and Ida Zacher Darr, Joe Leuthold, and Eldon Metzger via an easy ridge from Tenmile Pass.
Morning Star Peak is a 6,020 ft (1,830 m) mountain summit located near the western edge of the North Cascades, in Snohomish County of Washington state. It is situated 2.5 mi (4.0 km) southwest of Barlow Pass along the Mountain Loop Highway near the Monte Cristo area. It is set on land managed by Mount Baker-Snoqualmie National Forest. The nearest higher neighbor is Sperry Peak, 1 mile (1.6 km) to the northwest. Precipitation runoff from the south side of the mountain drains into the Sultan River, and the north side drains into headwaters of the Stillaguamish River. July through September offer the most favorable weather for climbing this mountain.
Rock Mountain is a 6,840+ ft mountain summit located 6.3 mi (10.1 km) northeast of Stevens Pass in Chelan County of Washington state. This peak is situated north of U.S. Highway 2, approximately midway between Stevens Pass and Lake Wenatchee, on land managed by the Okanogan–Wenatchee National Forest. Rock Mountain is the second-highest point on Nason Ridge, following Mount Howard, 1.37 mi (2.20 km) to the northeast. Rock Mountain was named by Albert Hale Sylvester. Precipitation runoff from the peak drains into tributaries of the Wenatchee River.
Black Mountain is a 7,262-foot-elevation (2,213-meter) summit located in the North Cascades, in Snohomish County of Washington state. The mountain is situated in the Glacier Peak Wilderness on land managed by Mount Baker-Snoqualmie National Forest. Neighbors include line parent Kololo Peaks, 6 mi (9.7 km) to the east, Painted Mountain two miles west, and Glacier Peak is 5 mi (8.0 km) to the northeast. Precipitation runoff from the peak drains west into tributaries of the North Fork Sauk River, and east into the White Chuck River. Topographic relief is significant as the summit rises 3,460 feet above the White Chuck in two miles. The first ascent of the summit was likely made in 1897 by a survey team including A. H. Dubor, Thomas G. Gerdine, and Sam Strom, who named the mountain for the dark color of its rock. The ascent from the north via Lake Byrne is non-technical.
Painted Mountain is a 6,975-foot-elevation (2,126-meter) summit located in the North Cascades, in Snohomish County of Washington state. The mountain is situated in the Glacier Peak Wilderness on land managed by Mount Baker-Snoqualmie National Forest. Neighbors include line parent Black Mountain, 2.2 mi (3.5 km) to the east, and Glacier Peak is 7 mi (11 km) to the northeast. Precipitation runoff from the peak drains west into tributaries of the North Fork Sauk River. Topographic relief is significant as the summit rises nearly 5,000 feet above the river in less than two miles.
Wilmans Peaks is a 6,880-foot elevation (2,097 m) mountain summit, in Snohomish County of Washington state.