Petunia Peak | |
---|---|
Highest point | |
Elevation | 6,953 ft (2,119 m) [1] |
Prominence | 433 ft (132 m) [1] |
Isolation | 0.62 mi (1.00 km) [2] |
Coordinates | 47°50′04″N123°11′46″W / 47.834338°N 123.196105°W [3] |
Geography | |
Country | United States |
State | Washington |
County | Jefferson |
Protected area | Olympic National Park Buckhorn Wilderness |
Parent range | Olympic Mountains |
Topo map | USGS Mount Deception |
Geology | |
Rock age | Eocene |
Climbing | |
Easiest route | class 2 scrambling via Royal Lake [1] |
Petunia Peak is a 6,953-foot (2,119-metre) mountain summit located in Jefferson County of Washington state.
Petunia Peak is set in the northeastern Olympic Mountains, and is situated on the boundary shared by Olympic National Park with the Buckhorn Wilderness, on land partially managed by the Olympic National Forest. Precipitation runoff from Petunia Peak drains into tributaries of the Dungeness River, and topographic relief is significant as the east aspect rises 3,750 feet (1,143 m) above the river in approximately 1.7 mile, and the west aspect rises 2,000 feet above Royal Basin in less than one mile. Old-growth forests of Douglas fir, western hemlock, and western redcedar grow on the lower slopes surrounding the peak. Like the town of Sequim 17 miles to the north, Petunia Peak lies in the rain shadow of the Olympic Mountains. It is also called "Petunia Peaks", as a higher summit known as North Petunia Peak (6,998 ft) rises 0.6 mile (1 km) to the north. [4] [5] This landform's name has not been officially adopted by the U.S. Board on Geographic Names, so the mountain is not labeled on USGS maps.
Petunia Peak is located in the marine west coast climate zone of western North America. [6] 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. [7] 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. [7] The months July through September offer the most favorable weather for viewing or climbing this peak. [1]
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 Deception is a peak in the Olympic Mountains of Cascadia. It is in Olympic National Park on the Olympic Peninsula in the U.S. state of Washington.
Mount Townsend is a mountain in the U.S state of Washington located within the Buckhorn Wilderness near Quilcene.
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.
Mount Johnson is a summit in the Olympic Mountains and is located in Jefferson County of Washington state. It is situated within Olympic National Park and the Daniel J. Evans Wilderness. At 7,680 feet (2,341 m) high, Mount Johnson is the fourth-highest peak of the Olympic Mountains, after Mount Olympus, Mount Deception, and Mount Constance. It is the highest peak in The Needles range which is a subset of the Olympic range. The nearest higher neighbor is Mount Deception, 1.34 mi (2.16 km) to the south. Mount Johnson is set in the eastern portion of the Olympic Mountains within the drainage basin of the Dungeness River. This location puts it in the rain shadow of the Olympic Range, resulting in less precipitation than Mount Olympus and the western Olympics receive.
Mount Skokomish is a 6,434-foot (1,961 meter) mountain summit located in the Olympic Mountains, in Mason County of Washington state, United States. It is situated on the shared boundary of Olympic National Park with Mount Skokomish Wilderness, and it is the highest point of the wilderness. The nearest higher peak is Mount Stone, 1.66 mi (2.67 km) to the northeast. It is visible on the Olympic skyline from as far away as Seattle. Mt. Skokomish has three summits, the south peak being the highest. Precipitation runoff drains into the Hamma Hamma River and Skokomish River. Like the river, the mountain's toponym honors the Skokomish people.
Mount Fricaba is a 7,139-foot-elevation (2,176 m) double summit mountain located in the Olympic Mountains, in Jefferson County of Washington state. It is situated on the shared border of Olympic National Park with Buckhorn Wilderness, and is the highest point in that wilderness, as well as the Olympic National Forest. Its nearest higher peak is Hal Foss Peak, 0.74 miles (1.19 km) to the southwest. Precipitation runoff from the peak drains east into headwaters of the Dungeness River, or west into Deception Creek which is a tributary of the Dosewallips River. The mountain's name was officially adopted in 1961 by the United States Board on Geographic Names based on usage by The Mountaineers since 1907, and inclusion in Fred Beckey's "Climber's Guide to the Cascade and Olympic Mountains of Washington" published in 1949. The first ascent of the mountain was made in 1957 by Don Bechlem and Jack Newman.
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.
Martin Peak is a mountain summit in the Olympic Mountains and is located in Jefferson County of Washington state. It is located within Olympic National Park. At 7,638 feet (2,328 m) high, Martin Peak is the seventh-highest peak of the Olympic Mountains, and the second-highest peak in The Needles range, which is a subset of the Olympic range. Its nearest higher neighbor is Mount Johnson, 0.53 mi (0.85 km) to the north-northwest. Precipitation runoff from this peak drains west into headwaters of Gray Wolf River, or east into Royal Creek, both of which are part of the Dungeness River drainage basin. Martin Peak was given its name based on the first ascent in 1940 by George W. Martin (1901–1970), and Elvin Johnson.
Athena is a 7,365-foot-elevation (2,245 meter) mountain summit located within Olympic National Park in Jefferson County of Washington state. Athena is situated at the head of the Hoh Glacier, and the Hubert Glacier lies below the west aspect. Its neighbors include Mount Olympus, 1.7 mi (2.7 km) to the northwest, and Aries 1.7 mi (2.7 km) to the northeast. Athena has subpeaks "Athena II" (7,259 ft), and "Athena's Owl" (7,000 ft). Precipitation runoff from the mountain drains into the Queets and Hoh Rivers, with Athena being the highest point within the Queets drainage basin.
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.
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.
Tyler Peak is a 6,364 feet (1,940 m) mountain summit located in Clallam County of Washington state, United States. It is situated in the northeastern Olympic Mountains, near the northern end of Gray Wolf Ridge, and is set within Buckhorn Wilderness, on land managed by the Olympic National Forest. The next highest neighbor is Mt. Baldy, two miles to the west.
Hal Foss Peak is a 7,179-foot-elevation (2,188 m) mountain summit located in the Olympic Mountains, in Jefferson County of Washington state. It is situated within Olympic National Park, and the Daniel J. Evans Wilderness. The nearest higher neighbor is Mount Mystery, 0.6 miles (0.97 km) to the southwest, and Mount Fricaba is 0.74 miles (1.19 km) to the northeast. Precipitation runoff from the peak drains east to the Dungeness River via Heather Creek, and west into Deception Creek which is a tributary of the Dosewallips River. Topographic relief is significant as the summit rises 2,800 feet (853 m) above Heather Creek in approximately one mile.
Copper Mountain is a 5,425-foot (1,654 m) mountain summit located in the southeast portion of the Olympic Mountains, in Mason County of Washington state. It is situated on the boundary shared by Daniel J. Evans Wilderness and Mount Skokomish Wilderness, as well as the shared common border of Olympic National Park with Olympic National Forest. The nearest higher neighbor is Mount Ellinor, 1.67 miles (2.69 km) to the east. Wagonwheel Lake lies immediately north of the peak. Topographic relief is significant as the summit rises nearly 4,700 feet (1,433 m) above the Staircase Ranger Station at Lake Cushman in approximately 1.5 miles (2.4 km). Precipitation runoff from the mountain drains north into the Hamma Hamma River, and south into the North Fork Skokomish River, thence Lake Cushman.
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.
The Needles is a mountain ridge located within Olympic National Park in Jefferson County of Washington state.
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.
Maiden Peak is a 6,434-foot (1,961 m) summit located in Olympic National Park, in Clallam County of Washington state. It is part of the Olympic Mountains and is situated near the eastern end of Hurricane Ridge within the Daniel J. Evans Wilderness. The nearest higher neighbor is Elk Mountain, 1.62 mi (2.61 km) to the west-southwest, and Blue Mountain is set 3.14 mi (5.05 km) to the east-northeast. The peak is set approximately midway along the trail which connects Deer Park and Obstruction Point. Precipitation runoff from the south slope of the mountain drains into Grand Creek, whereas the north slope is drained by Maiden Creek, and all ultimately reaches the Strait of Juan de Fuca. Topographic relief is significant as the summit rises 3,000 feet (910 m) above Grand Creek in one mile. This landform's name was officially adopted in 1961 by the U.S. Board on Geographic Names. One story has the origin of the name being derived from nearby Maiden Lake where young men and women camped around 1913, and the other being from a group of hikers that passed this area.