Ludden Peak

Ludden Peak is a 5,854-foot (1,784-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state.[3] Ludden Peak is part of the Bailey Range, which is a subrange of the Olympic Mountains, and is set within the Daniel J. Evans Wilderness.[6] In clear weather, the mountain can be seen from the park's visitor center on Hurricane Ridge. The nearest higher neighbor is Mount Scott, one mile to the south-southeast, line parent Mount Ferry rises 1.6 mi (2.6 km) to the southwest, Dodger Point is 1.9 mi (3.1 km) to the northeast, and Stephen Peak is set 2.7 mi (4.3 km) to the northwest.[6] Precipitation runoff from the mountain drains into tributaries of the Elwha River.

Ludden Peak
North aspect (centered), from Hurricane Hill
Highest point
Elevation5,854 ft (1,784 m)[1]
Prominence694 ft (212 m)[1]
Parent peakMount Ferry (6,195 ft)[2]
Isolation1.16 mi (1.87 km)[2]
Coordinates47°51′22″N 123°32′25″W[3]
Naming
EtymologyAddison "Doc" Ludden
Geography
Ludden Peak is located in Washington (state)
Ludden Peak
Ludden Peak
Location of Ludden Peak in Washington
Ludden Peak is located in the United States
Ludden Peak
Ludden Peak
Ludden Peak (the United States)
LocationOlympic National Park
Jefferson County, Washington, US
Parent rangeOlympic Mountains
Topo mapUSGS Mount Queets
Geology
Age of rockEocene
Type of rockMetaconglomerate[4]
Climbing
First ascentUnknown[1]
Easiest routeclass 2 via Dodger Point[5]

Etymology

This peak was originally named "Mount Squire" by the 1889–90 Seattle Press Expedition after Watson Carvosso Squire, US Senator from the state of Washington. However, this geographical feature's name was officially adopted by the U.S. Board on Geographic Names to remember Addison "Doc" Ludden (1851–1927), an early pioneer of the Elwha Valley.[7] Ludden had a mining claim and cabin near the peak. He was buried at Ocean View Cemetery in Port Angeles, Washington.

Climate

Based on the Köppen climate classification, Ludden Peak is located in the marine west coast climate zone of western North America.[8] 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 October offer the most favorable weather for viewing and climbing.[1]

Geology

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust.[9] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times. Ludden Peak is composed of hardened metaconglomerate.

  • Ludden Peak in upper left
    Ludden Peak in upper left
  • Ludden Peak centered in the distance, viewed from Hurricane Ridge. (Dodger Point on left, Mt. Ferry to right)
    Ludden Peak centered in the distance, viewed from Hurricane Ridge. (Dodger Point on left, Mt. Ferry to right)

See also

References
  1. "Ludden Peak – Climbers Guide to the Olympic Mountains". climbersguideolympics.com. Retrieved January 19, 2022.
  2. "Ludden Peak – 5,854' WA". listsofjohn.com. Retrieved January 18, 2022.
  3. "Ludden Peak". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved January 18, 2022.
  4. Daniel Mathews, 2021, Cascadia Revealed: A Guide to the Plants, Animals, and Geology of the Pacific Northwest Mountains, Timber Press, ISBN 9781643261010, page 531.
  5. Olympic Mountain Rescue, Climber's Guide to the Olympic Mountains, 1988, Mountaineers Books, ISBN 9780898861549, page 193.
  6. "Ludden Peak". Peakbagger.com.
  7. Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  8. 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.
  9. Alt, D.D.; Hyndman, D.W. (1984). Roadside Geology of Washington. pp. 249–259. ISBN 0-87842-160-2.
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