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Mountain in Washington (state), United States
Petunia Peak
North aspect
Highest point
Elevation6,953 ft (2,119 m)
Prominence433 ft (132 m)
Isolation0.62 mi (1.00 km)
Coordinates47°50′04″N 123°11′46″W / 47.834338°N 123.196105°W / 47.834338; -123.196105
Geography
Petunia Peak is located in Washington (state)
Petunia Peak
Petunia Peak
Location of Petunia Peak in Washington
Show map of Washington (state)
Petunia Peak is located in the——United States
Petunia Peak
Petunia Peak
Petunia Peak (the United States)
Show map of the United States
CountryUnited States
StateWashington
CountyJefferson
Protected areaOlympic National Park
Buckhorn Wilderness
Parent rangeOlympic Mountains
Topo mapUSGS Mount Deception
Geology
Age of rockEocene
Climbing
Easiest routeclass 2 scrambling via Royal Lake

Petunia Peak is a 6,953-foot (2,119-metre) mountain summit located in Jefferson County of Washington state.

Description

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. 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.

Climate

Petunia Peak is located in the marine west coast climate zone of western North America. 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. 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/no cloud cover during the summer. The months July through September offer the most favorable weather for viewing or climbing this peak.

Gallery

  • East aspect centered, from Marmot Pass. The Needles in upper left.
    East aspect centered, from Marmot Pass. The Needles in upper left.
  • North Petunia Peak and Petunia Peak seen from north. Mt. Deception upper right.
    North Petunia Peak and Petunia Peak seen from north. Mt. Deception upper right.
  • Petunia Peak (right) seen from east. Mt. Deception upper left corner.
    Petunia Peak (right) seen from east. Mt. Deception upper left corner.
  • North Petunia Peak (right of center) seen from Royal Basin. Petunia Peak in upper right corner of frame.
    North Petunia Peak (right of center) seen from Royal Basin.
    Petunia Peak in upper right corner of frame.
  • North Petunia Peak (left) and Petunia Peak
    North Petunia Peak (left) and Petunia Peak
  • Southwest aspect
    Southwest aspect

See also

References

  1. ^ Petunia Peak, climbersguideolympics.com
  2. ^ "Petunia Peak - 6,953' WA". listsofjohn.com. Retrieved 2022-02-04.
  3. ^ "Petunia Peak". Peakbagger.com.
  4. ^ Petunia Peaks, Mountaineers.org
  5. ^ "North Petunia Peak". Peakbagger.com.
  6. ^ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11. ISSN 1027-5606.
  7. ^ McNulty, Tim (2009). Olympic National Park: A Natural History. Seattle, Washington: University of Washington Press.

External links

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