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
Elevation	5,854 ft (1,784 m)[1]
Prominence	694 ft (212 m)[1]
Parent peak	Mount Ferry (6,195 ft)[2]
Isolation	1.16 mi (1.87 km)[2]
Coordinates	47°51′22″N 123°32′25″W[3]
Naming
Etymology	Addison "Doc" Ludden
Geography
Ludden Peak Location of Ludden Peak in Washington Show map of Washington (state) Ludden Peak Ludden Peak (the United States) Show map of the United States
Location	Olympic National Park Jefferson County, Washington, US
Parent range	Olympic Mountains
Topo map	USGS Mount Queets
Geology
Age of rock	Eocene
Type of rock	Metaconglomerate[4]
Climbing
First ascent	Unknown[1]
Easiest route	class 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.

Gallery

See also

• Olympic Mountains
• Geology of the Pacific Northwest

References

External links

• Doc Ludden: photo
• "Olympic National Park". National Park Service.
• Weather forecast: Ludden Peak
• Doc Ludden's homestead in Elwha Valley: photo
• Doc Ludden's cabin: Wikimedia photo