Mount Mathias

Mount Mathias is a 7,156-foot (2,181-metre) mountain summit located within Olympic National Park in Jefferson County of Washington state.^[4] Its nearest higher neighbor is Mount Olympus, 1.76 mi (2.83 km) to the east.^[1] Mount Mathias is wedged between the massive Blue Glacier below its west slope, and the Hoh Glacier on the east side. Precipitation runoff from the mountain drains into the Hoh River.

Mount Mathias
Mt. Mathias, from NNW
Highest point
Elevation	7,156 ft (2,181 m)[1]
Prominence	996 ft (304 m)[1]
Parent peak	Mount Olympus (7,980 ft)[1]
Isolation	0.97 mi (1.56 km)[2]
Coordinates	47°48′18″N 123°40′37″W[1]
Geography
Mount Mathias Location of Mount Mathias in Washington Show map of Washington (state) Mount Mathias Mount Mathias (the United States) Show map of the United States
Country	United States
State	Washington
County	Jefferson
Protected area	Olympic National Park
Parent range	Olympic Mountains
Topo map	USGS Mount Olympus
Geology
Rock age	Eocene
Climbing
First ascent	1957 by [3]
Easiest route	class 4 climbing via West Face[3]

History

This mountain was originally named "Apollo", for one of the Olympian deities in Greek and Roman mythology who made Mount Olympus home.^[5] It was renamed in honor of Francis Wayland "Matt" Mathias (1884–1959), a mountaineer, naturalist, and Grays Harbor County civic leader.^[5] The Mathias name was officially adopted in 1960 by the U.S. Board on Geographic Names.^[4]

The first ascent of this peak was made in 1957 by Yves Eriksson and Jim Hawkins.^[3]

Climate

Blue Glacier and Mount Mathias

Based on the Köppen climate classification, Mount Mathias is located in the marine west coast climate zone of western North America.^[6] 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.^[7] 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.^[7] The months of July through September offer the most favorable weather for viewing or climbing this peak.

Geology

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust.^[8] The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.

Mt.Mathias centered, Mt. Olympus to the right

See also

• Mountains portal

• Geology of the Pacific Northwest