Pyramid Peak (Pierce County, Washington)

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Pyramid Peak
Pyramid Peak 6937'.jpg
Pyramid Peak seen from the southeast
Highest point
Elevation 6,937 ft (2,114 m) [1]
Prominence 497 ft (151 m) [1]
Coordinates 46°48′25″N121°48′43″W / 46.8068426°N 121.8120695°W / 46.8068426; -121.8120695 Coordinates: 46°48′25″N121°48′43″W / 46.8068426°N 121.8120695°W / 46.8068426; -121.8120695 [2]
Geography
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Pyramid Peak
Location of Pyramid Peak in Washington
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Pyramid Peak
Pyramid Peak (the United States)
Location Mount Rainier National Park, Pierce County, Washington, U.S.
Parent range Cascades
Topo map USGS Mount Rainier West
Climbing
First ascent 1915 Mountaineers party. [3]
Easiest route Scrambling

Pyramid Peak is a 6,937-foot (2,114-metre) mountain summit located in Mount Rainier National Park in Pierce County of Washington state. [2] It is part of the Cascade Range and overlooks the Indian Henry's Hunting Ground. It is situated at the base of the Success Cleaver, south of South Tahoma Glacier, and southwest of Pyramid Glacier. The summit provides views of Mount Rainier, Mount Adams, Mount St. Helens, and peaks of the Tatoosh Range. Precipitation runoff from Pyramid Peak drains into Pyramid Creek, Tahoma Creek, and Fishers Horn Pipe Creek, which are all tributaries of the Nisqually River.

Mount Rainier National Park national park of the United States

Mount Rainier National Park is an American national park located in southeast Pierce County and northeast Lewis County in Washington state. The park was established on March 2, 1899 as the fifth national park in the United States, preserving 236,381 acres including all of Mount Rainier, a 14,411-foot (4,392 m) stratovolcano. The mountain rises abruptly from the surrounding land with elevations in the park ranging from 1,600 feet to over 14,000 feet (490–4,300 m). The highest point in the Cascade Range, Mount Rainier is surrounded by valleys, waterfalls, subalpine meadows, and 91,000 acres of old-growth forest. More than 25 glaciers descend the flanks of the volcano, which is often shrouded in clouds that dump enormous amounts of rain and snow.

Pierce County, Washington County in Washington

Pierce County is a county in the U.S. state of Washington. As of the 2010 Census, the population was 795,225, making it the second-most populous county in Washington behind King County, and the 63rd-most populous in the United States. The county seat and largest city is Tacoma. Formed out of Thurston County on December 22, 1852, by the legislature of Oregon Territory, it was named for U.S. President Franklin Pierce. Pierce County is in the Seattle metropolitan area.

Cascade Range mountain range in western North America

The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as the North Cascades, and the notable volcanoes known as the High Cascades. The small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains. The latter term is also sometimes used by Washington residents to refer to the Washington section of the Cascades in addition to North Cascades, the more usual U.S. term, as in North Cascades National Park. The highest peak in the range is Mount Rainier in Washington at 14,411 feet (4,392 m).

Contents

History

The descriptive name Pyramid Peak came from its pyramidal shape. An early writer described the peak as follows; "We had a better chance to observe Pyramid Peak in the morning light. It is in the form of a gigantic pyramid, perfect in outline. From a distance it appears to be black basalt, and on its sides no snow clings." [4] The name was officially adopted in 1913 by the United States Board on Geographic Names. [2]

United States Board on Geographic Names US geographic naming government agency

The United States Board on Geographic Names (BGN) is a federal body operating under the United States Secretary of the Interior. The purpose of the board is to establish and maintain uniform usage of geographic names throughout the federal government of the United States.

Climate

Pyramid Peak 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, 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 Cascades experiences high precipitation, especially during the winter months in the form of snowfall. 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.

North America Continent entirely within the Northern Hemisphere and almost all within the Western Hemisphere

North America is a continent entirely within the Northern Hemisphere and almost all within the Western Hemisphere. It is also considered by some to be a northern subcontinent of the Americas. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the west and south by the Pacific Ocean, and to the southeast by South America and the Caribbean Sea.

Weather front boundary separating two masses of air of different densities

A weather front is a boundary separating two masses of air of different densities, and is the principal cause of meteorological phenomena outside the tropics. In surface weather analyses, fronts are depicted using various colored triangles and half-circles, depending on the type of front. The air masses separated by a front usually differ in temperature and humidity.

Pacific Ocean Ocean between Asia and Australia in the west, the Americas in the east and Antarctica or the Southern Ocean in the south.

The Pacific Ocean is the largest and deepest of Earth's oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean in the south and is bounded by Asia and Australia in the west and the Americas in the east.

See also

Geology of the Pacific Northwest geology of Oregon and Washington (United States) and British Columbia (Canada)

The geology of the Pacific Northwest includes the composition, structure, physical properties and the processes that shape the Pacific Northwest region of the United States and Canada. The region is part of the Ring of Fire: the subduction of the Pacific and Farallon Plates under the North American Plate is responsible for many of the area's scenic features as well as some of its hazards, such as volcanoes, earthquakes, and landslides.

Pyramid Peak while descending from Mildred Point Pyramid Peak while descending from Mildred Point.jpg
Pyramid Peak while descending from Mildred Point

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Paul Bunyans Stump

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Pyramid Peak (Whatcom County, Washington)

Pyramid Peak is a 7,182-foot (2,189-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.

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Mount Fremont

Mount Fremont is a 7,317 feet (2,230 m) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Sourdough Mountains, a subset of the Cascade Range. Mount Fremont is situated northwest of the Sunrise Historic District, with a popular trail leading to the Mount Fremont Fire Lookout. However, this trail does not reach the true summit, and access is further limited by snowpack closing the Sunrise Road much of the year. July, August, and September are typically the months when the Sunrise Road is seasonally open for vehicle traffic. Second Burroughs Mountain is its nearest higher peak, 1.31 mi (2.11 km) to the southwest. Precipitation runoff from Mount Fremont drains into the White River.

Marcus Peak

Marcus Peak is a 6,962 feet (2,122 m) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Sourdough Mountains, a subset of the Cascade Range and is situated north of Dege Peak. The peak was named in 1932 for Marcus Whitman (1802–1847), an early pioneer and physician. The Whitman Glacier on Little Tahoma also honors him. Access to Marcus Peak is limited due to snow closing the Sunrise Road much of the year. July, August, and September are typically the months when the Sunrise Road is seasonally open for vehicle traffic. The nearest higher peak is Palisades Peak, 0.64 miles (1.03 km) to the north-northeast. Precipitation runoff from Marcus Peak drains into the White River.

Yakima Peak mountain in Washington, United States of America

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Deadwood Peak

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Tamanos Mountain

Tamanos Mountain is a 6,790 feet (2,070 m) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range. Tamanos Mountain is situated west of Governors Ridge and northeast of the Cowlitz Chimneys, all of which can be seen from the Sunrise Historic District. The name tamanos derives from Chinook Jargon and has the meaning of guardian spirit. The normal climbing access is from the Owyhigh Lakes Trail, and from the lakes scramble up the south slope to the summit.

Cowlitz Chimneys

Cowlitz Chimneys are a group of four rhyolite towers located in Mount Rainier National Park in Pierce County of Washington state. As part of the Cascade Range, the Cowlitz Chimneys are situated southwest of Tamanos Mountain and east of Banshee Peak, all of which are visible from the Sunrise Historic District. The Sarvant Glacier is set on the north aspect of these remnants of a volcanic plug. Cowlitz is the name of several geographical features in Mount Rainier National Park, as well as the state of Washington. The name appeared as early as the Lewis and Clark journals of 1805 when it was written as "Cowliskee" and has the Chinook Jargon meaning of "capturing the medicine spirit".

Barrier Peak

Barrier Peak is a small 6,521 ft summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range and is situated west of Cayuse Pass, 0.53 mile west-northwest of Buell Peak, and 0.4 mile south-southwest of Governors Ridge, which is its nearest higher peak. The normal climbing access is from the Owyhigh Lakes Trail. The peak was so named because it served as a barrier between the Cayuse Pass region and the rest of Mount Rainier National Park.

Mount Ruth (Washington)

Mount Ruth is an 8,690 ft summit located within Mount Rainier National Park in Pierce County of Washington state. Part of the Cascade Range, Mount Ruth is situated between the Emmons Glacier and the Inter Glacier. Access is via the Glacier Basin Trail. The name of the peak honors Ruth Knapp, daughter of the prospector who built Knapp's Cabin in Glacier Basin below the peak. Precipitation runoff from Mount Ruth drains into the White River.

Denman Peak mountain in Washington, United States of America

Denman Peak is a small 6,006 ft summit in the Tatoosh Range which is a sub-range of the Cascade Range. It's located south of Mount Rainier within Mount Rainier National Park. Denman Peak is situated east of Lane Peak and west of Pinnacle Peak.

Buell Peak

Buell Peak is a small 5,756 ft summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range and is situated 1.5 miles southwest of Cayuse Pass and 0.53 mile east-southeast of Barrier Peak, which is its nearest higher peak. The normal climbing access is from the Owyhigh Lakes Trail. The peak's name honors John Latimore Buell who arrived in Orting, Washington in 1890 and went into the hardware business.

Pinnacle Peak (Whatcom County, Washington)

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.

Skyscraper Mountain

Skyscraper Mountain is a 7,078 feet (2,157 m) summit located in Mount Rainier National Park in Pierce County of Washington state. It is part of the Cascade Range. Skyscraper Mountain is situated northwest of the Sunrise Historic District, from which a four-mile hike leads to the mountain, mostly on the Wonderland Trail. However, the trail does not reach the summit, but it is still a walk up to the top from Skyscraper Pass. The summit provides views of Burroughs Mountain, Sluiskin Mountain, and Mount Rainier. Mount Fremont is its nearest higher peak, 1.1 mi (1.8 km) to the east. Access is limited by snowpack closing the Sunrise Road much of the year. July, August, and September are typically the months when the Sunrise Road is seasonally open for vehicle traffic. Precipitation runoff from Skyscraper Mountain drains into tributaries of the White River.

References

  1. 1 2 "Pyramid Peak, Washington". Peakbagger.com.
  2. 1 2 3 "Pyramid Peak". Geographic Names Information System . United States Geological Survey . Retrieved 2019-09-24.
  3. 1 2 Beckey, Fred W. Cascade Alpine Guide, Climbing and High Routes. Seattle, WA: Mountaineers Books, 2008.
  4. Mount Rainier National Park Place Names. Gary Fuller Reese (author), 2009.