Warrior Peak | |
---|---|
Highest point | |
Elevation | 7,320+ ft (2,230+ m) [1] |
Prominence | 760 ft (232 m) [1] |
Parent peak | Inner Constance [2] |
Isolation | 0.83 mi (1.34 km) [2] |
Coordinates | 47°47′03″N123°08′01″W / 47.78411°N 123.133549°W [1] |
Geography | |
Country | United States |
State | Washington |
County | Jefferson |
Protected area | Olympic National Park |
Parent range | Olympic Mountains |
Topo map | USGS Mount Deception |
Geology | |
Rock age | Eocene |
Rock type | pillow basalt |
Climbing | |
First ascent | 1945 Fred Beckey (solo) |
Easiest route | Scrambling class 3 [3] |
Warrior Peak is a 7,320+ ft (2,230+ m) double summit mountain located in Olympic National Park and Jefferson County of Washington state. Warrior is the 11th-highest peak in the Olympic Mountains. [1] The southeast summit is the slightly higher of the two summits, the northwest peak is estimated at 7,285 feet elevation. [3] Precipitation runoff from the west side of the mountain drains into Home Creek, a tributary of the Dungeness River, whereas the east side drains into Tunnel Creek which is a tributary of the Big Quilcene River. Warrior Peak is easy to identify from Seattle, since it appears as the first prominent peak immediately north of Mount Constance, which is the dominant peak on the skyline. Warrior's nearest higher peak is Mount Constance, 0.8 mi (1.3 km) to the south-southeast. [1] The first ascent of the mountain was made in 1945 by Fred Beckey, who solo climbed both summits, and named the mountain. [3]
Based on the Köppen climate classification, Warrior Peak is located in the marine west coast climate zone of western North America. [4] Weather fronts originating in the Pacific Ocean travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing them to drop their moisture in the form of rain or snow. As a result, the Olympics experience high precipitation, especially during the winter months in the form of snowfall. [5] Because of maritime influence, snow tends to be wet and heavy, resulting in avalanche danger. 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] The months of July through September offer the most favorable weather for climbing the mountain. [3]
The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust. [6] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.
Mount Constance is a peak in the Olympic Mountains of Washington and the third highest in the range. It is the most visually prominent peak on Seattle's western skyline. Despite being almost as tall as the ice-clad Mount Olympus to the west, Mount Constance has little in the way of glaciers and permanent snow because the eastern, and particularly this northeastern, portion of the Olympics receives far less precipitation. However the narrow and steep Crystal Glacier still exists on the mountain's north face, shaded by the bulk of the main peak and with a small lake at its terminus. In addition, the treeline is higher here than mountains to the west, also hinting at the drier alpine conditions.
Mount Mystery is a prominent 7,639-foot (2,328-metre) mountain summit located in the Olympic Mountains in Jefferson County of Washington state. It is located within Olympic National Park on the Olympic Peninsula. Mount Mystery is the sixth-highest peak of the Olympic Mountains, after Mount Olympus, Mount Deception, Mount Constance, Mount Johnson, and Inner Constance. Its nearest higher neighbor is Mount Deception, 1.32 mi (2.12 km) to the north-northwest. Little Mystery (6,941 ft) is a subsidiary summit south of Mount Mystery.
Inner Constance is a summit of the Olympic Mountains and is located in Jefferson County of Washington state. It is located near the eastern edge of Olympic National Park on the Olympic Peninsula. At 7,670 feet (2,338 m), Inner Constance is the fifth-highest peak of the Olympic Mountains, after Mount Olympus, Mount Deception, Mount Constance, and Mount Johnson. Its nearest higher neighbor is Mount Constance, 0.9 mi (1.4 km) to the east. Within this nearly mile-wide separation resides a deep glacially carved canyon called "Avalanche Canyon". Precipitation runoff on the north side of the peak drains into tributaries of the Dungeness River, whereas the south side drains into tributaries of the Dosewallips River.
Mount Tom is a remote 7,076-foot (2,157-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. The nearest higher neighbor is Mount Olympus, 1.76 mi (2.83 km) to the east. Due to heavy winter snowfalls, Mount Tom supports the massive White Glacier on its northeast slope, despite its modest elevation. This glacier is the westernmost glacier in the contiguous states, and the summit is the westernmost peak higher than 7000+ feet elevation. Precipitation runoff from the mountain drains into tributaries of the Hoh River.
White Mountain is a 6,378-foot (1,944-metre) mountain summit located in the Olympic Mountains, in Jefferson County of Washington state. Situated in Olympic National Park, its nearest higher neighbor is Mount LaCrosse, 0.95 mi (1.53 km) to the northeast, and an unnamed glacier lies in the north cirque between the two peaks. The Anderson massif lies 3.1 mi (5.0 km) to the north of White Mountain. Precipitation runoff from the mountain drains into tributaries of the Quinault River and Duckabush River.
Sentinel Peak is a 6,592-foot-high (2,009 m) mountain summit located in the Olympic Mountains, in Jefferson County of Washington state. Rising in the center of Olympic National Park, its nearest higher neighbor is Mount Fromme, 1.42 miles (2.29 km) to the northwest. Sentinels Sister is a lower 6,301-foot-high (1,921 m) companion summit situated 0.65 miles (1.05 km) to the southwest. The two peaks stand as sentinels above the Dosewalips Valley and Hayden Pass, and were possibly named by an early expedition of the Seattle Mountaineers. Precipitation runoff from the peak drains to Hood Canal via the Dosewallips River.
Boulder Ridge is a 6,852-foot (2,088-metre) elevation mountain ridge located in the eastern Olympic Mountains in Jefferson County of Washington state. It is set within Buckhorn Wilderness on land managed by the Olympic National Forest. The nearest higher neighbor is Alphabet Ridge, 0.94 mi (1.51 km) to the south, and Buckhorn Mountain rises 1.3 mi (2.1 km) to the north. Precipitation runoff from Boulder Ridge drains east into headwaters of the Big Quilcene River, west into tributaries of Dungeness River, and south into Charlia Lakes, thence Tunnel Creek.
Mount Ferry is a 6,195-foot (1,888-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. Mount Ferry is the eighth-highest peak in the Bailey Range, which is a subrange of the Olympic Mountains. In clear weather, the mountain can be seen from the visitor center at Hurricane Ridge. Its nearest higher neighbor is Mount Pulitzer, 0.6 mi (0.97 km) to the southwest. Stephen Peak is set 2.26 mi (3.64 km) to the northwest, and Mount Olympus is 7.2 mi (11.6 km) to the southwest. Precipitation runoff from the mountain drains into tributaries of the Elwha and Hoh Rivers.
Mount Worthington is a 6,938-foot (2,115-metre) elevation double-summit mountain located in the eastern Olympic Mountains in Jefferson County of Washington state. It is set within Buckhorn Wilderness, on land managed by the Olympic National Forest. The nearest neighbor is Iron Mountain, 0.76 mi (1.22 km) to the southwest, and the nearest higher peak is Buckhorn Mountain, 1.3 mi (2.1 km) to the southwest. Precipitation runoff from Mount Worthington drains south into the Big Quilcene River, or north into Copper Creek which is a tributary of the Dungeness River. This mountain was first known as Copper Peak, but was renamed by Jack Christensen for the William J. Worthington family, pioneers of nearby Quilcene. Copper was mined in the Tubal Cain mine at the northern base of this mountain in the early 1900s. In the same vicinity of the abandoned mine are the remains of a modified B-17 plane that crashed on January 19, 1952, when returning from a search-and-rescue mission.
Muncaster Mountain is a 5,910-foot (1,801-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. It is situated 4.4 mi (7.1 km) south-southeast of Mount Christie, and 14.6 mi (23.5 km) southeast of Mount Olympus. Precipitation runoff from the mountain drains into Rustler Creek, which is a tributary of the Quinault River. Although modest in elevation, relief is significant as the summit rises 4,000 feet above the Rustler Creek valley in one mile.
Mount Noyes is a 6,173-foot (1,882 m) mountain summit located deep within Olympic National Park in Jefferson County of Washington state. Part of the Olympic Mountains, Mount Noyes is situated seven miles southeast of Mount Olympus, and set within the Daniel J. Evans Wilderness. The nearest higher neighbor is Mount Meany, 0.6 miles (0.97 km) to the north, and Mount Seattle rises one mile to the southeast. Noyes is a major triple divide point with precipitation runoff from the mountain draining east into the headwaters of the Elwha River, west into headwaters of Saghalie Creek which is a tributary of the Queets River, and south into headwaters of Seattle Creek which is a tributary of the Quinault River. Topographic relief is significant as the east, west, and south aspects of the peak each rise 2,200 feet (670 m) in approximately one mile.
Mount Seattle is a 6,246-foot (1,904-metre) mountain summit deep within Olympic National Park in Jefferson County of Washington state. Part of the Olympic Mountains, Mount Seattle is situated 7.5 miles southeast of Mount Olympus, and set within the Quinault Rainforest and Daniel J. Evans Wilderness. The nearest higher neighbor is Mount Meany, 1.65 miles (2.66 km) to the north-northwest, and Mount Noyes rises one mile to the northwest. Precipitation runoff from the mountain drains north into headwaters of the Elwha River, and south into tributaries of the Quinault River. Topographic relief is significant as the northeast aspect of the peak rises over 3,800 feet (1,200 m) above the Elwha valley in approximately 1.5-mile. Low Divide forms the saddle between Mt. Seattle and Mount Christie.
Mount Wilder is a 5,939-foot (1,810-metre) mountain summit located near the head of the Elwha Valley, deep within Olympic National Park in Jefferson County of Washington state. Part of the Olympic Mountains, Wilder represents the southernmost peak of the Bailey Range. It is situated 8.7 miles east-southeast of Mount Olympus, and is set within the Daniel J. Evans Wilderness. Neighbors include line parent Mount Dana, 2.3 miles (3.7 km) to the northeast, and Mount Seattle rises 3.7 miles to the southwest. The headwaters of the Goldie River form on the south slope of the mountain, and precipitation runoff from the mountain drains into Goldie River and other tributaries of the Elwha River. Topographic relief is significant as the south aspect of the peak rises nearly 3,800 feet (1,160 m) in less than two miles.
Mount Delabarre is a remote 6,024-foot (1,836-metre) mountain summit deep within Olympic National Park in Jefferson County of Washington state. Part of the Olympic Mountains, Mount Delabarre is 12.4 miles southeast of Mount Olympus, set within the Daniel J. Evans Wilderness. The nearest higher neighbor is line parent Mount Christie, 2.5 miles to the west-northwest. Precipitation runoff from the mountain drains north into headwaters of Delabarre Creek, which is a tributary of the Elwha River, and south into Rustler Creek, which is a tributary of the North Fork Quinault River. Topographic relief is significant as the southwest aspect of the peak rises 3,400 feet (1,036 m) above Rustler Creek in approximately one mile.
Welch Peaks is a 6,110-foot (1,862-metre) mountain in the eastern Olympic Mountains in Jefferson County of Washington state, United States. It is set within Buckhorn Wilderness, on land managed by the Olympic National Forest. The nearest higher neighbor is Mount Townsend, 1.2 mi (1.9 km) to the north, and Mount Worthington rises 2.1 mi (3.4 km) to the southwest. Precipitation runoff from Welch Peaks drains into tributaries of the Big Quilcene River, and Silver Creek which is a tributary of the Dungeness River. Topographic relief is significant as the summit rises 3,100 feet (945 m) above Townsend Creek in approximately one mile. The mountain's toponym was officially adopted in 1963 by the U.S. Board on Geographic Names.
Cat Peak is a 5,940-foot (1,811-metre) mountain summit within Olympic National Park in Clallam County of Washington state.
Mount Scott is a 5,913-foot (1,802-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state.
Mount Fromme is a 6,705-foot (2,044-metre) mountain summit in Olympic National Park in Jefferson County of Washington state. It is situated at the head of Dosewallips River, within the Daniel J. Evans Wilderness. The nearest higher neighbor is Mount Claywood, 0.6 mi (0.97 km) to the northwest. Other nearby peaks include Lost Peak, 1.8 mi (2.9 km) to the northeast, and Sentinel Peak, 1.4 mi (2.3 km) to the southeast. Precipitation runoff from the mountain drains east into headwaters of the Dosewallips River, and west into Hayes River, which is a tributary of the Elwha River. Topographic relief is significant as the summit rises 2,250 feet (685 m) above Dose Meadows in approximately one mile.
Jefferson Peak is a 5,720-foot (1,743 m) mountain summit located in the Olympic Mountains in Mason County of Washington state. It is situated in the Mount Skokomish Wilderness, on land managed by Olympic National Forest. The mountain's toponym honors Thomas Jefferson (1743–1826), the third president of the United States. The nearest higher neighbor is line parent Mount Pershing, 1.3 mi (2.1 km) to the southwest. Precipitation runoff drains into Jefferson Creek and the Hamma Hamma River. Topographic relief is significant as the north aspect rises over 4,100 feet (1,200 m) above the Hamma Hamma valley in approximately one mile.
Iron Mountain is a 6,826-foot (2,081-metre) elevation summit located in the eastern Olympic Mountains in Jefferson County of Washington state. It is set within Buckhorn Wilderness, on land managed by Olympic National Forest. It is situated between Buckhorn Mountain, 0.58 mi (0.93 km) to the southwest, and Mount Worthington, 0.76 mi (1.22 km) to the northeast. Precipitation runoff from Iron Mountain drains south into the Big Quilcene River, and north into Copper Creek which is a tributary of the Dungeness River. Topographic relief is significant as the southeast aspect rises 2,800 feet above the Big Quilcene River in less than one mile, and the north aspect rises 1,700 feet above Buckhorn Lake in one-half mile. Old-growth forests of Douglas fir, western hemlock, and western redcedar grow in the valleys surrounding the peak. The nearest community is Quilcene 11 miles to the east.