Paul Bunyans Stump | |
---|---|
Highest point | |
Elevation | 7,480 ft (2,280 m) [1] |
Prominence | 920 ft (280 m) [1] |
Parent peak | Neve Peak (7,505 ft) [1] |
Isolation | 0.91 mi (1.46 km) [2] |
Coordinates | 48°39′58″N121°09′00″W / 48.666026°N 121.150049°W [1] |
Geography | |
Location | North Cascades National Park Whatcom County Washington, U.S. |
Parent range | North Cascades Cascade Range |
Topo map | USGS Diablo Dam |
Climbing | |
First ascent | August 2, 1931 by William Degenhardt, Herbert Strandberg [3] |
Easiest route | class 3 Scrambling |
Paul Bunyans Stump is a 7,480+ ft (2,280+ m) mountain summit in the North Cascades Range of Washington, United States. [4] It is located within North Cascades National Park. It rises steeply from Diablo Lake, one of the reservoirs on the Skagit River. It is part of a group of peaks that form the northern end of a chain running south through climbing destinations such as Colonial Peak and Snowfield Peak. The nearest peak to Paul Bunyans Stump is Pinnacle Peak, 0.37 mi (0.60 km) to the north, and the nearest higher peak is Neve Peak, 0.9 mi (1.4 km) to the southeast. Like many North Cascade peaks, Paul Bunyans Stump is more notable for its large, steep rise above local terrain than for its absolute elevation. Precipitation runoff from the mountain drains into Diablo Lake and Skagit River.
Paul Bunyans Stump was first climbed on August 2, 1931 by William Degenhardt and Herbert Strandberg of the Seattle Mountaineers. They called it "What's the Matterhorn." [3]
Paul Bunyans Stump is located in the marine west coast climate zone of western North America. [3] 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 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 North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. [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. [5] Because of maritime influence, snow tends to be wet and heavy, resulting in high avalanche danger. [5]
The North Cascades features some of the most rugged topography in the Cascade Range with craggy peaks, spires, 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.
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 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.
Colonial Peak is a mountain in the North Cascades of Washington, United States. It rises steeply from the southwest bank of Thunder Arm of Diablo Lake, one of the artificial reservoirs on the Skagit River. It is part of a group of peaks that form the northern end of a chain running south through prized climbing destinations such as Eldorado Peak, Forbidden Peak, and Goode Mountain. Colonial Peak takes its name from the Colonial mining claim on its slopes.
Snowfield Peak is in North Cascades National Park in the U.S. state of Washington. Located in the south unit of the park, Snowfield Peak is .70 mi (1.13 km) east of the summit known as Horsemans Pack and the Neve Glacier descends from the north slopes of the mountain.
Graybeard Peak is a 7,965-foot (2,428-metre) mountain summit located in Skagit County, Washington.
Ruby Mountain is a prominent 7,412-foot (2,259-metre) mountain summit located in the North Cascades Range of Washington state. It is situated in Ross Lake National Recreation Area which is part of the North Cascades National Park Complex. The Diablo Lake Overlook along the North Cascades Highway is at the foot of the mountain. The nearest higher peak is Colonial Peak, 4.2 miles (6.8 km) to the southwest. Precipitation runoff on the east side of the mountain drains into Ross Lake via Ruby Creek, whereas the west side of the mountain drains into Diablo Lake via Thunder Creek. Topographic relief is significant as the summit rises 6,200 feet above Diablo Lake in approximately two miles.
Pyramid Peak is a 7,189-foot (2,191-metre) mountain summit in the North Cascades Range of Washington, United States. It is located within North Cascades National Park. It rises steeply from Diablo Lake, one of the reservoirs on the Skagit River. It is part of a group of peaks that form the northern end of a chain running south through climbing destinations such as Colonial Peak, Paul Bunyans Stump, and Snowfield Peak. Like many North Cascade peaks, Pyramid Peak is more notable for its large, steep rise above local terrain than for its absolute elevation. Precipitation runoff from the mountain drains into Diablo Lake and Skagit River.
The Triplets is a 7,240+ ft summit located in Skagit County of Washington state. This breccia triple pinnacle is part of the North Cascades Range. The Triplets is situated above Cascade Pass on the shared border of North Cascades National Park and Glacier Peak Wilderness. The nearest higher neighbor is Cascade Peak, 0.35 miles (0.56 km) to the west-northwest. Surface runoff from the mountain drains into the Cascade River.
Mix-up Peak, also known as Mixup Peak, is a 7,440-foot (2,270-metre) mountain summit located on the shared boundary of Skagit County and Chelan County in Washington state. It is part of the North Cascades Range and is situated one mile south of Cascade Pass on the shared border of North Cascades National Park and Glacier Peak Wilderness. The nearest higher peak is Magic Mountain, 1.02 miles (1.64 km) to the east-southeast. Mix-up Peak is at the northern end of the Ptarmigan Traverse which is an alpine route to remote mountains such as Mount Formidable and Dome Peak. The Cache Glacier occupies a cirque below its eastern flank. Surface runoff on the east side the mountain drains into the Stehekin River, whereas precipitation runoff drains into the Cascade River from the west side.
McKay Ridge is a 7,000+ ft ridge located in Whatcom County in Washington state. It is part of the Okanogan Range which is a sub-range of the North Cascades. It's situated north of the North Cascades Highway on land administered by the Okanogan–Wenatchee National Forest. The nearest higher peak is Majestic Mountain, 1.6 miles (2.6 km) to the northeast. Precipitation runoff from the ridge drains into Ross Lake via tributaries of the Skagit River.
Helen Buttes are two prominent summits near the western edge of the North Cascades, in Skagit County of Washington state. It's located four miles northwest of Marblemount, Washington in the Noisy-Diobsud Wilderness. It is situated on land administered by the Mount Baker-Snoqualmie National Forest. The nearest higher peak is Diobsud Buttes, 3.11 miles (5.01 km) to the north. Precipitation runoff from Helen Buttes drains into tributaries of the Skagit River.
Diobsud Buttes are summits near the western edge of the North Cascades, in Skagit County of Washington state. It's located north of Marblemount, Washington, and Helen Buttes, along the shared boundary of North Cascades National Park and the Noisy-Diobsud Wilderness. The nearest higher peak is Logger Butte, 0.85 mi (1.37 km) to the north. Precipitation runoff from Diobsud Buttes drains into tributaries of the Skagit River.
Porcupine Peak is a 7,762-foot-elevation (2,366-meter) mountain located in Skagit County of Washington state.
Molar Tooth is a 7,547-foot-elevation (2,300-meter) granite summit located on the shared border of Okanogan County and Skagit County, in Washington state. The mountain is part of the Okanagan Range which is a subset of the Cascade Range. Set in the Okanogan–Wenatchee National Forest, Molar Tooth is situated south of Cutthroat Pass, and 0.57 miles (0.92 km) north of Cutthroat Peak, which is also its nearest higher peak. The easiest climbing route is class 4 scrambling, but solid rock provides class 5 technical routes as well. Precipitation runoff from the east side of Molar Tooth drains into tributaries of the Methow River, whereas runoff from the west side drains into tributaries of the Skagit River.
Red Mountain is a 7,662 feet (2,335 m) summit in the North Cascades Range of Washington, United States. It is located in Skagit County and within North Cascades National Park and the Stephen Mather Wilderness. It is situated on a smooth ridge of brick-red color at the western culmination of Ragged Ridge.
Round Mountain is a 5,320+ ft mountain summit at the western edge of the North Cascades, in Skagit County of Washington state. It is located nine miles northwest of Darrington, Washington and is situated on land administered by the Mount Baker-Snoqualmie National Forest. Round Mountain is remarkable for its 4,780 feet of prominence which ranks as the most in Skagit County, and eighth most of all the mountains in Washington state. The nearest higher peak is Whitehorse Mountain, 7.85 miles (12.63 km) to the south-southeast. Precipitation runoff from Round Mountain drains into tributaries of the Stillaguamish River.
Mount Chaval is a craggy 7,127-foot (2,172-metre) mountain summit located in Skagit County of Washington state. Situated within the Glacier Peak Wilderness, Mount Chaval is positioned west of the crest of the North Cascades Range, approximately 15 miles northeast of the town of Darrington. It has two subsidiary peaks, East Peak and Middle Peak, each 7040 ft. Its nearest higher neighbor is Snowking Mountain, 2.51 miles (4.04 km) to the northeast. Precipitation runoff from Mount Chaval drains into tributaries of the Skagit 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 Range, 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 (7425 ft), and Middle Peak (7400 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.
Tricouni Peak is an 8,102-foot (2,469-metre) mountain summit located in Skagit County of Washington state. It is situated in North Cascades National Park, north of the North Klawatti Glacier and southeast of the Borealis Glacier. Its nearest higher peak is Primus Peak, 0.54 mi (0.87 km) to the west. Precipitation runoff from Tricouni drains into Thunder Creek. The peak is named for the tricouni which was used for traction on ice, and the approach to the peak involves traversing a glacier.
The Chopping Block is a 6,819-foot (2,078-metre) mountain summit located in the Picket Range within North Cascades National Park in the state of Washington. The mountain is officially named Pinnacle Peak on maps, but hardly anyone calls it by that name. The nearest higher peak is Mount Degenhardt, 0.6 mi (0.97 km) to the northeast. The Chopping Block can be seen from the North Cascades National Park Newhalem visitor center, weather permitting. Precipitation runoff from the peak drains into Goodell Creek, a tributary of the Skagit River.
Pinnacle Peak is a 7,360+ ft mountain summit in the North Cascades Range of Washington, United States. It is located within North Cascades National Park, between Pyramid Peak and Paul Bunyans Stump, which is the nearest higher peak. It rises steeply from Diablo Lake, one of the reservoirs on the Skagit River. It is part of a group of peaks that form the northern end of a chain running south through climbing destinations such as Colonial Peak and Snowfield Peak. Like many North Cascade peaks, Pinnacle Peak is more notable for its large, steep rise above local terrain than for its absolute elevation. Precipitation runoff from the mountain drains into Diablo Lake and Skagit River. The approach is via the Pyramid Lake Trail, starting near Diablo Dam on the North Cascades Highway. From the lake, there is route-finding up Pyramid Arm to Colonial Glacier.
Syncline Mountain is a 7,560-foot (2,300-metre) mountain summit located on the shared border between Okanogan County and Whatcom County in Washington state. It is part of the Okanogan Range, which is a sub-range of the North Cascades, and is situated on land managed by the Okanogan–Wenatchee National Forest. Its nearest neighbor is Tatie Peak, 0.8 miles (1.3 km) to the north, and the nearest higher neighbor is Mount Ballard, 2.1 miles (3.4 km) to the west. The Pacific Crest Trail traverses the east slope of the peak, with an off-trail scramble to reach the summit. Precipitation runoff from Syncline Mountain drains east into Trout Creek which is a tributary of the Methow River, or northwest into Slate Creek, which is part of the Skagit River drainage basin. This unofficially named mountain features a conspicuous syncline, hence its descriptive name.