Mount Delabarre

{{Infobox mountain

| name = Mount Delabarre

| photo = Mount Delabarre.jpg

| photo_caption = Ice-clad Delabarre, north aspect

| elevation_ft = 6024

| elevation_ref =[http://www.climbersguideolympics.com/peaks/quinault-group/mount-delabarre-mount-taylor Mount Delabarre, climbersguideolympics.com]

| prominence_ft = 1140

| prominence_ref =

| isolation_mi = 2.56

| isolation_ref ={{cite web|url=https://listsofjohn.com/peak/50406|title=Delabarre, Mount – 6,024' WA|website=listsofjohn.com|accessdate=2022-01-11}}

| parent_peak = Mount Christie (6,181 ft)

| etymology = W. R. Delabarre

| country = United States

| state = Washington

| region = Jefferson

| region_type = County

| part_type = Protected area | part = Olympic National Park

| range = Olympic Mountains

| map = Washington#USA

| map_caption = Location of Mt. Delabarre in Washington

| label_position = bottom

| coordinates = {{coord|47.68625|N|123.49339|W|type:mountain_region:US-WA_scale:100000_source:gnis|format=dms|display=inline,title}}

| coordinates_ref =

| topo = USGS Chimney Peak

| rock =

| age = Eocene

| first_ascent = Unknown

| easiest_route = {{YDS|3}} scrambling

}}

Mount Delabarre is a remote {{Convert|6024|ft|m|abbr=off|adj=on}} mountain summit deep within Olympic National Park in Jefferson County of Washington state. Part of the Olympic Mountains, Mount Delabarre is 12.4 miles southeast of Mount Olympus, set within the Daniel J. Evans Wilderness. The nearest higher neighbor is line parent Mount Christie, 2.5 miles to the west-northwest.{{cite peakbagger|988|Mount Delabarre, Washington}} Precipitation runoff from the mountain drains north into headwaters of Delabarre Creek, which is a tributary of the Elwha River, and south into Rustler Creek, which is a tributary of the North Fork Quinault River. 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.Olympic Mountain Rescue, Olympic Mountains: A Climbing Guide, 4th Edition, 2006, Mountaineers Books, {{ISBN|9780898862065}}, page 206. 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.{{cite book |last=Parratt |first=Smitty |title=Gods and Goblins: A Field Guide to Place Names of Olympic National Park |edition=1st |year=1984}}{{cite gnis|id=1518663|name=Delabarre Creek|accessdate=2022-01-11}}

The mountain is also called "Mount Taylor", 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.

Climate

Based on the Köppen climate classification, Mount Delabarre is located in the marine west coast climate zone of western North America.{{cite journal | author = Peel, M. C. |author2=Finlayson, B. L. |author3=McMahon, T. A. | year = 2007 | title = Updated world map of the Köppen−Geiger climate classification | journal = Hydrol. Earth Syst. Sci. | volume = 11 | pages = 1633–1644 | issn = 1027-5606}} 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.{{cite book|last=McNulty|first=Tim|title=Olympic National Park: A Natural History|year=2009|publisher=University of Washington Press|location=Seattle, Washington}} 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. The months July and August offer the most favorable weather for climbing this mountain.

Geology

The Olympic Mountains are composed of obducted clastic wedge material and oceanic crust, primarily Eocene sandstone, turbidite, and basaltic oceanic crust.{{cite book|last=Alt|first=D.D.|author2=Hyndman, D.W.|year=1984|title=Roadside Geology of Washington|pages=249–259|isbn=0-87842-160-2}} The mountains were sculpted during the Pleistocene era by erosion and glaciers advancing and retreating multiple times.

References

External links

{{cite web |url=http://www.nps.gov/olym| url-status=live | archive-url=https://ghostarchive.org/archive/20220104/http://www.nps.gov/olym| archive-date=2022-01-04 |title=Olympic National Park |publisher=National Park Service}}{{cbignore}}
[https://www.yr.no/en/forecast/daily-table/2-5792180/United%20States/Washington/Jefferson/Delabarre%20Creek Weather forecast]
Aerial photo: [https://pbase.com/image/87774331 PBase]
Aerial photo: [https://www.flickr.com/photos/ancientambler/8977865416/in/photolist-eFkUB3-9gwVnX-yFZQz-dYr3tV-dYr3qB-a9mRqW-5tsCRb-NivA2W-odYprr-otnxGS-ow6vnf-oeqGVp-oewZZb-6RxToM-8qMA1o-dXqJXb-r2vv4d-otzyC6-DLvqEV-vYNja-oc5MA9-pV6XYu-6P2Vgi-6P2VxF-6P74xJ-qcEYNa-otingM-ovHkeU-orxDWu-2MZ8AV-2MWQyt-ourSy7-8XSJY6-29H54D6-a9mRF7-otzxQz-trfYbw-a9jqdK-odAcL7-otdHAj-6P74g7-p5Kz5n-9YXxb8-a4vVpb-2FHYP4-aAjBAw-oeNE63-odAh4N-GmrxC2-6RBUA5 Flickr]

{{Geographic Location 2

| Center = Mount Delabarre

| North = Mount Wilder

| Northeast = Crystal Peak

| East = Chimney Peak

| Southeast =

| South = Muncaster Mountain

| Southwest = Rustler Creek

| West = Mount Christie

| Northwest = Mount Seattle

}}

Delabarre