Steeple Rock (Washington)

Last updated
Steeple Rock
Steeple Rock 5288' on Hurricane Ridge.jpg
Steeple Rock seen from the east
Highest point
Elevation 5,567 ft (1,697 m) [1]
Prominence 567 ft (173 m) [1]
Coordinates 47°57′43″N123°27′15″W / 47.961935°N 123.454043°W / 47.961935; -123.454043 [1]
Geography
USA Washington relief location map.jpg
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Steeple Rock
Location of Steeple Rock in Washington
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Steeple Rock
Steeple Rock (the United States)
CountryUnited States
State Washington
County Clallam
Protected area Olympic National Park
Parent range Olympic Mountains
Topo map USGS Mount Angeles
Geology
Age of rock Eocene
Type of rock Basalt
Climbing
Easiest route Scrambling class 3

Steeple Rock [2] is a 200-foot (61 meter) basalt pillar in the Olympic Mountains, and is located in Clallam County of Washington state. It rises next to the Obstruction Point Road on Hurricane Ridge within Olympic National Park. It's situated midway between Eagle Point and the Hurricane Ridge Visitor Center. Precipitation runoff drains into tributaries of the Elwha River and Morse Creek, thence to the Strait of Juan de Fuca.

Contents

Climate

Set in the north-central portion of the Olympic Mountains, Steeple Rock is located in the marine west coast climate zone of western North America. [3] 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. [4] 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. [4]

Geology

The Olympic Mountains are made up of obducted clastic wedge material and oceanic crust. They are primarily Eocene sandstones, turbidites, and basaltic oceanic crust. [5] Unlike the Cascades, the Olympic Mountains are not volcanic, and contain no granite. [4]

Millions of years ago, vents and fissures opened under the Pacific Ocean and lava flowed forth, creating huge underwater mountains and ranges called seamounts. The Farallon tectonic plate that formed a part of the Pacific Ocean floor (separate from the Pacific plate) inched eastward toward North America about 35 million years ago and most of the sea floor subducted beneath the continental land mass of the North America plate. Some of the sea floor, however, was scraped off and jammed against the mainland, creating the dome that was the forerunner of today's Olympics. Thrust-faulting northeast into the Vancouver Island/North Cascades corner pushes Olympic rock upward and southwestward, resulting in strata that appear to be standing on edge and that intermix with strata of different mineral composition. [4] All this occurred under water; the Olympics began to rise above the sea only 10–20 million years ago. [4]

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<span class="mw-page-title-main">Elk Mountain (Clallam County, Washington)</span> Mountain in Washington (state), United States

Elk Mountain is a 6,773-foot elevation (2,064 m) mountain summit located in the Olympic Mountains, in Clallam County of Washington state. It is set within Olympic National Park and is situated at the eastern end of Hurricane Ridge. The nearest higher peak is McCartney Peak, 5.12 mi (8.24 km) to the south-southwest. Precipitation runoff from the south slope of the mountain drains into tributaries of the Dungeness River, whereas the north slope is drained by tributaries of Morse Creek which thence empties into the Strait of Juan de Fuca.

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Trappers Peak is a 5,966-foot (1,818 m) elevation mountain summit located in the North Cascades of Washington state. It is situated within North Cascades National Park, Stephen Mather Wilderness, and Whatcom County. It rises steeply above Lower Thornton Lake which is set at the southwestern face of the mountain. Like many North Cascades peaks, Trappers Peak is more notable for its large, steep rise above local terrain than for its absolute elevation. Topographic relief is significant as the southeast aspect rises 5,500 feet (1,700 m) above the North Cascades Highway in approximately two miles. The nearest higher neighbor is Thornton Peak, 1.5 miles (2.4 km) to the northwest, Mount Triumph is two miles to the northwest, and Newhalem is three miles to the east-southeast. Precipitation runoff from the mountain drains into tributaries of the Skagit River. The summit of Trappers Peak is known for its grand view of the jagged peaks of the Picket Range.

<span class="mw-page-title-main">Maiden Peak (Washington)</span> Mountain in Washington (state), United States

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.

References

  1. 1 2 3 "Steeple Rock". Peakbagger.com.
  2. "Steeple Rock". Geographic Names Information System . United States Geological Survey, United States Department of the Interior . Retrieved 2018-08-07.
  3. 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.
  4. 1 2 3 4 5 McNulty, Tim (2009). Olympic National Park: A Natural History. Seattle, Washington: University of Washington Press.
  5. Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN   0-87842-160-2.