Mount Delabarre

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Coordinates: 47°41′11″N 123°29′36″W / 47.68625°N 123.49339°W / 47.68625; -123.49339
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Mount Delabarre
Ice-clad Delabarre, north aspect
Highest point
Elevation6,024 ft (1,836 m)[1]
Prominence1,140 ft (350 m)[1]
Parent peakMount Christie (6,181 ft)[2]
Isolation2.56 mi (4.12 km)[2]
Coordinates47°41′11″N 123°29′36″W / 47.68625°N 123.49339°W / 47.68625; -123.49339[1]
Naming
EtymologyW. R. Delabarre
Geography
Mount Delabarre is located in Washington (state)
Mount Delabarre
Mount Delabarre
Location of Mt. Delabarre in Washington
Mount Delabarre is located in the United States
Mount Delabarre
Mount Delabarre
Mount Delabarre (the United States)
CountryUnited States
State
class 3 scrambling[1]

Mount Delabarre is a remote 6,024-foot (1,836-metre) mountain summit deep within

Topographic relief
is significant as the southwest aspect of the peak rises 3,400 feet (1,036 m) above Rustler Creek in approximately one mile.

History

The mountain is named after W. R. Delabarre, the Port Angeles banker who provided financial assistance for The Mountaineers' 1907 exploration into the Olympic Mountains, which included the first ascent of Mount Olympus.[4] At a later time, Delabarre and Asahel Curtis scouted a different trail to Mt. Olympus, and in the course of their journey, the men crossed the stream that would later officially bear his name.[5][6]

The mountain is also called "Mount Taylor",[1] but neither name has been officially adopted by the United States Board on Geographic Names, so the peak is not labelled on USGS maps.

Two scramble routes to the summit have been established: via Martins Park trail, and via Godkin-Rustler Pass.[1]

Climate

Based on the

marine west coast climate zone of western North America.[7] 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.[8] 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.[8] The months July and August offer the most favorable weather for climbing this mountain.[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.

See also

References

  1. ^ a b c d e f g h Mount Delabarre, climbersguideolympics.com
  2. ^ a b "Delabarre, Mount – 6,024' WA". listsofjohn.com. Retrieved January 11, 2022.
  3. ^ "Mount Delabarre, Washington". Peakbagger.com.
  4. ISBN 9780898862065
    , page 206.
  5. ^ Parratt, Smitty (1984). Gods and Goblins: A Field Guide to Place Names of Olympic National Park (1st ed.).
  6. ^ "Delabarre Creek". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved January 11, 2022.
  7. ISSN 1027-5606
    .
  8. ^ a b McNulty, Tim (2009). Olympic National Park: A Natural History. Seattle, Washington: University of Washington Press.
  9. ISBN 0-87842-160-2
    .

External links
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