Gilhooley Tower is a basalt spire in the Olympic Mountains and is located in Jefferson County of Washington state. It is situated in Olympic National Park on the Olympic Peninsula. Its nearest higher peak is Mount Deception at 0.13 mi (0.21 km) to the southeast.[1] Precipitation runoff drains into tributaries of the Dungeness River and Dosewallips River.

Gilhooley Tower
Gilhooley Tower
Highest point
Elevation7,480 ft (2,280 m)[1]
Prominence120 ft (37 m)[1]
Parent peakMount Deception[2]
Isolation0.25 mi (0.40 km)[2]
Coordinates47°48′58″N 123°14′14″W / 47.816135°N 123.237232°W / 47.816135; -123.237232[1]
Geography
Gilhooley Tower is located in Washington (state)
Gilhooley Tower
Gilhooley Tower
Location of Gilhooley Tower in Washington
Gilhooley Tower is located in the United States
Gilhooley Tower
Gilhooley Tower
Gilhooley Tower (the United States)
CountryUnited States
StateWashington
CountyJefferson
Protected areaOlympic National Park
Parent rangeOlympic Mountains
Topo mapUSGS Mount Deception
Geology
Rock ageEocene
Rock typeBasalt
Climbing
First ascent1963 by Donald Anderson, Harold Pinsch, Joyce Pinsch[3]
Easiest routeClimbing class 4[2]

Climate

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Based on the Köppen climate classification, Gilhooley Tower is located in the marine west coast climate zone of western North America.[4] 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.[5] 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.[5]

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References

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  1. ^ a b c d "Gilhooley Tower". Peakbagger.com.
  2. ^ a b c "Gilhooley Tower - 7,540' WA". listsofjohn.com. Retrieved 2024-04-14.
  3. ^ "First Ascents – Climbers Guide to the Olympic Mountains". climbersguideolympics.com. Retrieved 2018-07-31.
  4. ^ 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.
  5. ^ a b McNulty, Tim (2009). Olympic National Park: A Natural History. Seattle, Washington: University of Washington Press.
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