Mount Seattle (Washington)

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Mount Seattle
Mount Seattle, Olympic National Park.png
East aspect
Highest point
Elevation 6,246 ft (1,904 m) [1]
Prominence 726 ft (221 m) [1]
Parent peak Mount Meany (6,695 ft) [2]
Isolation 1.65 mi (2.66 km) [2]
Coordinates 47°43′52″N123°34′39″W / 47.7309736°N 123.5776235°W / 47.7309736; -123.5776235 Coordinates: 47°43′52″N123°34′39″W / 47.7309736°N 123.5776235°W / 47.7309736; -123.5776235 [3]
Geography
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Mount Seattle
Location of Mt. Seattle in Washington
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Mount Seattle
Mount Seattle (the United States)
Location Olympic National Park
Jefferson County, Washington, US
Parent range Olympic Mountains
Topo map USGS Mount Christie
Geology
Age of rock Eocene
Climbing
First ascent 1907 by Asahel Curtis
Easiest route class 3 scrambling [1]

Mount Seattle is a 6,246-foot (1,904-metre) mountain summit located deep within Olympic National Park in Jefferson County of Washington state. [3] 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 mile (2.6 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 (1,160 m) above the Elwha valley in approximately 1.5 mile. Low Divide forms the saddle between Mt. Seattle and Mount Christie.

Contents

History

The mountain was named on April 29, 1890, by James Halbold Christie, leader of the 1889-90 Seattle Press Expedition, and Charles Adams Barnes, the expedition's topographer. Christie was sponsored by the Seattle newspaper Press, and named the mountain in honor of the city of Seattle. Observations from Mount Seattle enabled Barnes to finally complete his map of the Olympic Mountains. [4]

The first documented ascent of the summit was made in 1907 by Asahel Curtis, Grant Humes, and Lorenz Nelson who were reconnoitering for The Mountaineers first ascent attempt at Mount Olympus. [1] Three scramble routes to the summit have been established: via Noyes Basin, via Seattle Creek Basin, and via Low Divide. [1]

Climate

Based on the Köppen climate classification, Mount Seattle is located in the marine west coast climate zone of western North America. [5] Most weather fronts originate in the Pacific Ocean, and travel east toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks of the Olympic Range, causing them to drop their moisture in the form of rain or snowfall (Orographic lift). As a result, the Olympics experience high precipitation, especially during the winter months. 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. The months June through August offer the most favorable weather for viewing or climbing this mountain. [1]

Geology

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.

See also

Related Research Articles

Olympic Mountains Mountain range in Washington, United States

The Olympic Mountains are a mountain range on the Olympic Peninsula of the Pacific Northwest of the United States. The mountains, part of the Pacific Coast Ranges, are not especially high – Mount Olympus is the highest at 7,965 ft (2,428 m); however, the eastern slopes rise out of Puget Sound from sea level and the western slopes are separated from the Pacific Ocean by the low-lying 20 to 35 km wide Pacific Ocean coastal plain. The western slopes are the wettest place in the 48 contiguous states. Most of the mountains are protected within the bounds of Olympic National Park and adjoining segments of the Olympic National Forest.

Olympic Peninsula Peninsula in Washington, United States

The Olympic Peninsula is a large arm of land in western Washington that lies across Puget Sound from Seattle, and contains Olympic National Park. It is bounded on the west by the Pacific Ocean, the north by the Strait of Juan de Fuca, and the east by Hood Canal. Cape Alava, the westernmost point in the contiguous United States, and Cape Flattery, the northwesternmost point, are on the peninsula. Comprising about 3,600 square miles (9,300 km2), the Olympic Peninsula contained many of the last unexplored places in the contiguous United States. It remained largely unmapped until Arthur Dodwell and Theodore Rixon mapped most of its topography and timber resources between 1898 and 1900.

Mount Christie (Washington)

Mount Christie is high peak in the Olympic Mountains of Washington in Olympic National Park. Mount Christie is located in the Queets-Quinault group. Precipitation on Mt. Christie drains into the Elwha River on the north side, and into the Quinault River on the south side. The mountain was named to honor James Halbold Christie, who was the leader of the Seattle Press Expedition which first explored the unknown interior of the range in 1889–1890. The massif has several peaks, and the large Christie Glacier resides in the north cirque below the main summit.

Mount Angeles

Mount Angeles is located just south of Port Angeles, Washington in the Olympic National Park. It is the highest peak in the Hurricane Ridge area. The summit, which offers panoramic views of the Strait of Juan de Fuca and many of the peaks of the interior Olympic Mountains can be climbed from the Klahane Ridge trail.

Mount Meany

Mount Meany is a prominent 6,695-foot (2,041-metre) mountain summit located deep within Olympic National Park in Jefferson County of Washington state. With a good eye and clear weather, the top of the mountain can be seen from the visitor center at Hurricane Ridge. The nearest neighbor is Mount Noyes less than one mile to the south, and the nearest higher peak is Circe (6,847 ft) on Mount Olympus, 4.07 mi (6.55 km) to the northwest. There are scrambling routes on the east side, via Noyes-Meany col, and via the ridge from Mount Queets. Due to heavy winter snowfalls, Mount Meany supports several small glaciers on its north and east slopes, despite its modest elevation. Precipitation runoff from the mountain drains into the headwaters of both the Elwha and Queets Rivers.

Mount Tom (Washington)

Mount Tom is a remote 7,076-foot (2,157-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. Its 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.

West Peak (Jefferson County, Washington)

West Peak is a 7,365-foot-high (2,245 m) peak in the Olympic Mountains, in Jefferson County of Washington state. Rising in the center of Olympic National Park, it is the highest peak on the Anderson Massif. West Peak is the hydrographic apex of the Olympic Mountains, with precipitation runoff flowing outward to the Pacific Ocean via Quinault River, the Strait of Juan de Fuca via Elwha River, and Hood Canal via the Dosewallips River. The Eel Glacier is situated in a cirque east of the summit, and an unnamed glacier resides in the south cirque. Its nearest higher peak is Mount Mystery, 7.73 miles (12.44 km) to the northeast. The first ascent of the peak was made in 1930 by E. B. Hamilton. Legend has it that the mountain's name is for Mr. West, a participant in the 1890 O'Neil Expedition, rather than for its apparent position on the Anderson Massif. The West Branch of the Quinault River was named after him in 1890.

Stephen Peak

Stephen Peak is a 6,418-foot (1,956-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. Stephen Peak is the fifth-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, appearing to the left of Mount Olympus. Mount Ferry is set 2.26 mi (3.64 km) to the southeast, and Stephen's nearest higher neighbor is Ruth Peak which is an outlier of Mount Carrie, 2.1 mi (3.4 km) to the northwest. Precipitation runoff from the mountain drains into tributaries of the Elwha River and Hoh River. The first ascent of this peak was made in 1961 by Kent Heathershaw, Doug Waali, and Robert Wood.

Mount Ferry

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 Pulitzer (Washington)

Mount Pulitzer, also known as Snagtooth, is a 6,283-foot (1,915-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. Mount Pulitzer is the sixth-highest peak in the Bailey Range, which is a subrange of the Olympic Mountains. Its nearest neighbor is Mount Ferry, 0.58 mi (0.93 km) to the northeast, and its nearest higher neighbor is Stephen Peak, 2.58 mi (4.15 km) to the north. Mount Olympus is set 6.8 mi (10.9 km) to the southwest. In clear weather, the mountain can be seen from the visitor center at Hurricane Ridge. Precipitation runoff from the mountain drains into tributaries of the Elwha and Hoh Rivers.

Muncaster Mountain

Muncaster Mountain is a 5,910-foot (1,800-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 Claywood

Mount Claywood is a 6,836-foot (2,084-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. It is situated at the head of Lost River, and 15 mi (24 km) east of Mount Olympus. Its nearest higher neighbor is Mount Cameron, 2.4 mi (3.9 km) to the northeast. Other nearby peaks include Mt. Fromme, 0.58 mi (0.93 km) to the southeast, and Sentinel Peak, 2 mi (3.2 km) also to the southeast. Precipitation runoff from the mountain drains north and west into tributaries of the Elwha River, and east into Claywood Lake, thence Dosewallips River.

Woden - The Valhallas

Woden is a 6,038-foot (1,840-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state. Its nearest higher neighbor is Mount Tom, 3 mi (4.8 km) to the north-northwest, and Mount Olympus rises 3.8 mi (6.1 km) to the north-northeast. Woden is the highest point in The Valhallas, a sub-range south of Mount Olympus. Precipitation runoff from the mountain drains into tributaries of the South Fork Hoh River and Queets River. The Geri-Freki Glacier, which descends north from Woden. is the only glacier in The Valhallas.

Athena (Olympic Mountains)

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.

Chimney Peak (Olympic Mountains)

Chimney Peak is a 6,917-foot-elevation (2,108 meter) mountain summit located within Olympic National Park in Jefferson County of Washington state. Chimney Peak is situated near the head of Elwha Valley, and immediately north above Enchanted Valley. Topographic relief is significant as the southeast aspect rises 4,800 feet (1,463 meters) above Enchanted Valley in less than one mile. Enchanted Valley is also known as Valley of 10,000 Waterfalls, and numerous waterfalls tumble down the immense cliffs of Chimney Peak. Neighbors include Crystal Peak, 2.2 mi (3.5 km) to the north, White Mountain 3.5 mi (5.6 km) to the east, and West Peak 3.4 mi (5.5 km) to the northeast. Precipitation runoff from the mountain drains north to the Elwha River, and south to the Quinault River.

Crystal Peak (Olympic Mountains)

Crystal Peak is a 6,896-foot-elevation (2,102 meter) mountain summit located within Olympic National Park in Jefferson County of Washington state. Crystal Peak is situated two miles north of Enchanted Valley, near the heads of Hayes River and Quinault River. Topographic relief is significant as the northeast aspect rises 3,300 feet (1,006 meters) above Hayes River in less than one mile. Precipitation runoff from the mountain drains north to the Elwha River via Hayes River and Godkin Creek. Neighbors include line parent Chimney Peak, 2.2 mi (3.5 km) to the south, and proximate parent West Peak, 2.0 mi (3.2 km) to the east. The lower slopes of the mountain are surrounded by Western Red Cedar, Sitka Spruce, Western Hemlock, Alaskan Cedar, Mountain Hemlock, and Douglas-fir of the Quinault Rainforest.

Mount Noyes (Washington)

Mount Noyes is a 6,173-foot (1,882-metre) 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 mile 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 Lincoln (Washington)

Mount Lincoln is a 5,868-foot-elevation mountain summit located in 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. Lincoln is the second-highest point on Sawtooth Ridge, and the nearest higher neighbor is Mount Cruiser, 1.1 mi (1.8 km) to the northeast. Lincoln has two sub-peaks: a North Peak (5,690 ft/1,734 m), and a Southwest Peak (5,486 ft/1,672 m). Flapjack Lakes lie immediately west below the north sub-peak. Topographic relief is significant as the summit rises over 5,100 feet (1,555 m) above the Staircase Ranger Station at Lake Cushman in approximately two miles. Precipitation runoff from the mountain drains into tributaries of the North Fork Skokomish River, and partly into Mildred Lakes, thence Hamma Hamma River.

Mount Wilder

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 Mountain summit in Washington state

Mount Delabarre is a remote 6,024-foot (1,836-metre) mountain summit located deep within Olympic National Park in Jefferson County of Washington state. Part of the Olympic Mountains, Mount Delabarre is situated 12.4 miles southeast of Mount Olympus, and is 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.

References

  1. 1 2 3 4 5 6 Mount Seattle, climbersguideolympics.com
  2. 1 2 "Seattle, Mount - 6,246' WA". listsofjohn.com. Archived from the original on 2022-01-04. Retrieved 2022-01-04.
  3. 1 2 "Mount Seattle". Geographic Names Information System . United States Geological Survey . Retrieved 2022-01-04.
  4. Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  5. Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11: 1633–1644. ISSN   1027-5606.
  6. Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN   0-87842-160-2.