Mount Hood
Template:Short description Template:About Template:Use mdy dates Template:Good article Template:Infobox mountain
Mount Hood, also known as Wy'east, is an active stratovolcano in the Cascade Range and is a member of the Cascade Volcanic Arc. It was formed by a subduction zone on the Pacific Coast and rests in the Pacific Northwest region of the United States. It is located about Template:Cvt east-southeast of Portland, on the border between Clackamas and Hood River counties, and forms part of the Mount Hood National Forest. Much of the mountain outside the ski areas is part of the Mount Hood Wilderness. With a summit elevation of 11,249 ft (3,429 m),<ref name="ngs">Template:Cite ngs</ref> it is the highest mountain in the U.S. state of Oregon and is the fourth highest in the Cascade Range.<ref name="Swanson">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Ski areas on the mountain include Timberline Lodge ski area which offers the only year-round lift-served skiing in North America, Mount Hood Meadows, Mount Hood Skibowl, Summit Ski Area, and Cooper Spur ski area. Mt. Hood attracts an estimated 10,000 climbers a year.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The peak is home to 12 named glaciers and snowfields. Mount Hood is considered the Oregon volcano most likely to erupt.<ref>Most likely to erupt based on history; see {{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The odds of an eruption in the next 30 years are estimated at between 3 and 7%, so the U.S. Geological Survey (USGS) characterizes it as "potentially active", but the mountain is informally considered dormant.<ref name="USGS Hazards">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
EstablishmentsEdit
Timberline Lodge is a National Historic Landmark located on the southern flank of Mount Hood just below Palmer Glacier, with an elevation of about Template:Cvt.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The mountain has four ski areas: Timberline, Mount Hood Meadows, Ski Bowl, and Cooper Spur. They total over Template:Cvt of skiable terrain; Timberline, with one lift having a base at nearly Template:Cvt, offers the only year-round lift-served skiing in North America.<ref name="summerski">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
There are a few remaining shelters on Mount Hood still in use today. Those include the Coopers Spur, Cairn Basin, and McNeil Point shelters as well as the Tilly Jane A-frame cabin. The summit was home to a fire lookout in the early 1900s; however, the lookout did not withstand the weather and no longer remains today.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Mount Hood is within the Mount Hood National Forest, which comprises Template:Cvt of land, including four designated wilderness areas that total Template:Cvt, and more than Template:Cvt of hiking trails.<ref name="hoodfacts1">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The most northwestern pass around the mountain is called Lolo Pass. Native Americans crossed the pass while traveling between the Willamette Valley and Celilo Falls.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
NamingEdit
Indigenous namesEdit
It has been difficult to establish place names for Mount Hood that are of indigenous etymology, or to reconstruct names that may have been used prior to European contact.
Wy'eastEdit
The name Wy'east has been associated with Mount Hood for more than a century, but no evidence suggests that it is a genuine name for the mountain in any indigenous language. The name was possibly inspired by an 1890 work of author Frederic Balch, although Balch does not use it himself.<ref>Template:Cite news</ref><ref>Template:Cite journal</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The name may have been popularized by his story being combined with a play around 1911 at Pacific College. It is also possible it was 'invented' by scholars in the 20th century or even a minister hearing it second-hand around the same time the play was happening.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
In one version of Balch's story, the two sons of the Great Spirit Sahale fell in love with the beautiful maiden Loowit, who could not decide which to choose. The two braves, Wy'east and Pahto (unnamed in his novel, but appearing in a later adaptation), burned forests and villages in their battle over her. Sahale became enraged and smote the three lovers. Seeing what he had done, he erected three mountain peaks to mark where each fell. He made beautiful Mount St. Helens for Loowit, proud and erect Mount Hood for Wy'east, and the somber Mount Adams for the mourning Pahto.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
There are other versions of the legend. In another telling, Wy'east (Hood) battles Pahto (Adams) for the fair La-wa-la-clough (St. Helens). Or again Wy'east, the chief of the Multnomah tribe, competed with the chief of the Klickitat tribe. Their great anger led to their transformation into volcanoes. Their battle is said to have destroyed the Bridge of the Gods and thus created the great Cascades Rapids of the Columbia River.<ref>Template:Cite book</ref>
Other namesEdit
The mountain sits partly inside the reservation of the Confederated Tribes of Warm Springs, which comprises multiple languages including Sahaptin, Upper Chinook/Kiksht (Wasco) and Numu (Paiute). However, it has been difficult to determine names originating from these or other indigenous languages specifically referring to Mount Hood. Eugene Hunn suggests that the mountain may have lacked a specific name:<ref>Template:Cite book</ref>
Learning a landscape is not simply a matter of naming all the rivers and mountains... The Native American perspective emphasizes by contrast places as focal points of activity, places where significant human-landscape interactions occur. Thus, while a few prominent peaks may be given Indian names, such as taxùma [təqʷuʔməʔ] for Mt. Rainier (in the Puget Salish language) or lawilayt-łà [lawílatɬa], literally "the smoker," for Mt. St. Helens (in Sahaptin), other prominent peaks, e.g. Mts. Adams and Hood, are known simply as pàtu, a general term for snow-capped summit.
Current nameEdit
The mountain was given its present name on October 29, 1792, by Lt. William Broughton, a member of Captain George Vancouver's exploration expedition. Lt. Broughton observed its peak while at Belle Vue Point of what is now called Sauvie Island during his travels up the Columbia River, writing, "A very high, snowy mountain now appeared rising beautifully conspicuous in the midst of an extensive tract of low or moderately elevated land [location of today's Vancouver, Washington] lying S 67 E., and seemed to announce a termination to the river." Lt. Broughton named the mountain after Samuel Hood, 1st Viscount Hood, a British admiral.<ref name="Swanson"/>
Lewis and Clark spotted the mountain on October 18, 1805. A few days later at what would become The Dalles, Clark wrote, "The pinnacle of the round topped mountain, which we saw a short distance below the banks of the river, is South 43-degrees West of us and about Template:Cvt. It is at this time topped with snow. We called this the Falls Mountain, or Timm Mountain." Timm was the native name for Celilo Falls. Clark later noted that it was also Vancouver's Mount Hood.<ref name="firsttouch">Grauer, p. 9</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Two French explorers from the Hudson's Bay Company may have traveled into the Dog River area east of Mount Hood in 1818. They reported climbing to a glacier on "Montagne de Neige" (Mountain of Snow), probably Eliot Glacier.<ref name="firsttouch"/>
NamesakesEdit
,_crop.jpg){kind=link}
There have been two United States Navy ammunition ships named for Mount Hood. USS Mount Hood (AE-11) was commissioned in July 1944 and was destroyed in November 1944 while at anchor in Manus Naval Base, Admiralty Islands. Her explosive cargo ignited, resulting in 45 confirmed dead, 327 missing and 371 injured.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> A second ammunition ship, AE-29, was commissioned in May 1971 and decommissioned in August 1999.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Volcanic activityEdit
The glacially eroded summit area consists of several andesitic or dacitic lava domes; Pleistocene collapses produced avalanches and lahars (rapidly moving mudflows) that traveled across the Columbia River to the north. The eroded volcano has had at least four major eruptive periods during the past 15,000 years.<ref name=volcanoinformation>{{#invoke:citation/CS1|citation
|CitationClass=web
}}
Template:PD-notice</ref>
The last three eruptions at Mount Hood occurred within the past 1,800 years from vents high on the southwest flank and produced deposits that were distributed primarily to the south and west along the Sandy and Zigzag rivers. The volcano has had a VEI of 2 at least three times before.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The last eruptive period took place around 220 to 170 years ago, when dacitic lava domes, pyroclastic flows and mudflows were produced without major explosive eruptions. The prominent Crater Rock just below the summit is hypothesized to be the remains of one of these now-eroded domes. This period includes the last major eruption of 1781 to 1782 with a slightly more recent episode ending shortly before the arrival of the explorers Lewis and Clark in 1805. The latest minor eruptive event was thought to have occurred in August 1907,<ref name=volcanoinformation/><ref name="vulcan_hood">Template:Cite journal</ref> but has been discredited as "an observation of non-eruptive fumarolic activity." <ref name="eruptive_history">Template:Cite journal</ref>
The glaciers on the mountain's upper slopes may be a source of potentially dangerous lahars when the mountain next erupts. There are vents near the summit that are known for emitting gases such as carbon dioxide and sulfur dioxide.<ref name=lavadomes>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Prior to the 1980 eruption of Mount St. Helens, the only known fatality related to volcanic activity in the Cascades occurred in 1934, when a climber suffocated in oxygen-poor air while exploring ice caves melted by fumaroles in Coalman Glacier on Mount Hood.<ref name="Swanson"/>
Since 1950, there have been several earthquake swarms each year at Mount Hood, most notably in July 1980 and June 2002.<ref>Template:Cite gvp</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Seismic activity is monitored by the USGS Cascades Volcano Observatory in Vancouver, Washington, which issues weekly updates (and daily updates if significant eruptive activity is occurring at a Cascades volcano).<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The most recent evidence of volcanic activity at Mount Hood consists of fumaroles near Crater Rock and hot springs on the flanks of the volcano.<ref name="DONF">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Monitoring controversyEdit
A conflict exists between protecting public safety and protecting the environment. In 2014, a USGS employee, Dr. Seth Moran, proposed installing new instruments on Mount Hood to warn of volcanic activity. The instruments were installed at four different locations on the mountain, including:
- three seismometers to measure earthquakes
- three Global Positioning System (GPS) instruments to measure ground movement
- one instrument to measure gas emissions
The proposed locations were in a protected wilderness area, tightly controlled by the United States Forest Service. The project was opposed by Wilderness Watch, a conservation group.<ref>Template:Cite news</ref>
Three monitoring stations were eventually installed on Mount Hood in 2020.<ref>Template:Cite news</ref>
ElevationEdit
Mount Hood was first seen by European explorers in 1792 and is believed to have maintained a consistent summit elevation, varying by no more than a few feet due to mild seismic activity. Elevation changes since the 1950s are predominantly due to improved survey methods and model refinements of the shape of the Earth (see vertical reference datum). Despite the physical consistency, the estimated elevation of Mount Hood has varied substantially over the years, as seen in the following table:
| Date | Stated Elevation | Source | |
|---|---|---|---|
| 1854 | Template:Cvt | Thomas J. Dryer<ref name="grauer">Template:Cite book</ref> | |
| 1854 | Template:Cvt | Belden<ref name="grauer"/> | |
| 1857 | Template:Cvt | citation | CitationClass=web
}}</ref> |
| 1866 | Template:Cvt | Rev. Atkinson<ref name="grauer"/> | |
| 1867 | Template:Cvt | Col. Williamson<ref name="grauer"/> | |
| 1916 | Template:Cvt | Adm. Colbert<ref name="grauer"/> | |
| 1939 | Template:Cvt | Adm. Colbert<ref name="grauer"/> | |
| 1980 | Template:Cvt | USGS using NGVD 29<ref name="vulcan_hood"/> | |
| 1991 | Template:Cvt | U.S. National Geodetic Survey, 1986 measurement adjusted using NAVD 88<ref name="ngs"/> | |
| 1993 | Template:Cvt | Scientific expedition<ref name="Register" /> and Template:Cvt<ref name="Trafford" /> of slightly older origin | |
| 2008? | Template:Cvt | Encyclopedia Britannica<ref>Template:Cite encyclopedia</ref> |
Early explorers on the Columbia River estimated the elevation to be Template:Cvt. Two people in Thomas J. Dryer's 1854 expedition calculated the elevation to be Template:Cvt and the tree line to be at Template:Cvt. Two months later, a Mr. Belden claimed to have climbed the mountain during a hunting trip and determined it to be Template:Cvt upon which "pores oozed blood, eyes bled, and blood rushed from their ears." Sometime by 1866, Reverend G. H. Atkinson determined it to be Template:Cvt. A Portland engineer used surveying methods from a Portland baseline and calculated a height of between Template:Cvt. Many maps distributed in the late 19th century cited Template:Cvt, though Mitchell's School Atlas gave Template:Cvt as the correct value. For some time, many references assumed Mount Hood to be the highest point in North America.<ref name="grauer"/>
Modern height surveys also vary, but not by the huge margins seen in the past. A 1993 survey by a scientific party that arrived at the peak's summit with Template:Cvt of electronic equipment reported a height of Template:Cvt, claimed to be accurate to within Template:Cvt.<ref name="Register">Template:Cite news</ref> Many modern sources likewise list Template:Cvt as the height.<ref>Template:Cite book</ref><ref>Template:Cite book</ref><ref>Template:Cite book</ref> However, numerous others place the peak's height one foot lower, at Template:Cvt.<ref name="Trafford">Template:Cite book</ref><ref>Template:Cite book</ref><ref>Template:Cite journal</ref> Finally, a height of Template:Cvt has also been reported.<ref name="ngs" /><ref>Template:Cite book</ref><ref>Template:Cite book</ref><ref>Template:Cite news</ref>
GlaciersEdit
Template:GeoGroupMount Hood is host to 12<ref>{{#invoke:citation/CS1|citation
|CitationClass=web }}</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> named glaciers or snow fields, the most visited of which is Palmer Glacier, partially within the Timberline Lodge ski area and on the most popular climbing route. The glaciers are almost exclusively above the Template:Cvt level, which also is about the average tree line elevation on Mount Hood.<ref name="tree line">Template:Cite book</ref> More than 80 percent of the glacial surface area is above Template:Cvt.<ref name="gspp1365">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The glaciers and permanent snow fields have an area of Template:Cvt and contain a volume of about Template:Cvt. Eliot Glacier is the largest glacier by volume at Template:Cvt, and has the thickest depth measured by ice radar at Template:Cvt. The largest glacier by surface area is the Coe-Ladd Glacier system at Template:Cvt.<ref name="gspp1365" />
Glaciers and snowfields cover about 80 percent of the mountain above the Template:Cvt level. The glaciers declined by an average of 34 percent from 1907 to 2004. Glaciers on Mount Hood retreated through the first half of the 20th century, advanced or at least slowed their retreat in the 1960s and 1970s, and have since returned to a pattern of retreat.<ref>Template:Cite journal</ref> The neo-glacial maximum extents formed in the early 18th century.<ref name="Swanson" />
During the last major glacial event between 29,000 and 10,000 years ago, glaciers reached down to the Template:Cvt level, a distance of Template:Cvt from the summit. The retreat released considerable outwash, some of which filled and flattened the upper Hood River Valley near Parkdale and formed Dee Flat.<ref name="Swanson"/>
Older glaciation produced moraines near Brightwood and distinctive cuts on the southeast side; they may date to 140,000 years ago.<ref name="Swanson"/>
HikingEdit
Mt. Hood National Forest is home to approximately Template:Cvt of trails.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Cooper Spur Trail leads to Template:Cvt in elevation, the highest reachable point one can gain on the mountain without requiring mountaineering gear.
The Timberline Trail, which circumnavigates the entire mountain and rises as high as Template:Cvt, was built in the 1930s by the Civilian Conservation Corps. Typically, the Template:Cvt hike is snow-free from late July until the autumn snows begin. The trail includes over Template:Cvt of elevation gain and loss and can vary in distance year to year depending on river crossings. There are many access points, the shortest being a small walk from the Timberline Lodge. A portion of the Pacific Crest Trail is coincident with the Timberline Trail on the west side of Mount Hood.<ref name="timberlinetrail">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref name="gorp">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
The predecessor of the Pacific Crest Trail was the Oregon Skyline Trail, established in 1920, which connected Mount Hood to Crater Lake.<ref name=FS1921>Template:Cite book</ref>
ClimbingEdit
Mount Hood is Oregon's highest point and a prominent landmark visible up to Template:Cvt away. About 10,000 people attempt to climb Mount Hood each year.<ref name="goesright">Template:Cite news</ref> It has convenient access, though it presents some technical climbing challenges. There are no trails to the summit, with even the "easier" southside climbing route constituting a technical climb with crevasses, falling rocks, and often inclement weather. Ropes, ice axes, crampons and other technical mountaineering gear are necessary.<ref>Template:Cite news</ref> Peak climbing season is generally from April to mid-June.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
There are six main routes to approach the mountain, with about 30 total variations for summiting. The climbs range in difficulty from class 2 to class 5.9+ (for Acrophobia).<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The most popular route, dubbed the south route, begins at Timberline Lodge and proceeds up Palmer Glacier to Crater Rock, the large prominence at the head of the glacier. The route goes east around Crater Rock and crosses the Coalman Glacier on the Hogsback, a ridge spanning from Crater Rock to the approach to the summit. The Hogsback terminates at a bergschrund where the Coalman Glacier separates from the summit rock headwall. The route continues to the Pearly Gates, a gap in the summit rock formation, then right onto the summit plateau and the summit proper.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Technical ice axes, fall protection, and experience are now recommended in order to attempt the left chute variation or Pearly Gates ice chute. The Forest Service recommends several other route options due to these changes in conditions (e.g. "Old Chute," West Crater Rim, etc.).<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
Climbing accidentsEdit
{{#invoke:Labelled list hatnote|labelledList|Main article|Main articles|Main page|Main pages}}
As of May 2002, more than 130 people had died in climbing-related accidents since records have been kept on Mount Hood, the first in 1896.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Incidents in May 1986, December 2006, and December 2009 attracted intense national and international media interest. Though avalanches are a common hazard on other glaciated mountains, most Mount Hood climbing deaths are the result of falls and hypothermia.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }} </ref> Around 50 people require rescue per year.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> 3.4 percent of search and rescue missions in 2006 were for mountain climbers.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>
ClimateEdit
The summit of Mount Hood has a typical dry-summer alpine climate (Köppen: ETs), with temperatures below Template:Convert eight months of the year and no month with an average temperature above Template:Convert. Even in the hottest months, nightly average temperatures often dip below Template:Convert, and frost occurs almost every day, even in summer or the hottest time of year. Otherwise, all months have a dew point below Template:Convert. Template:Weather box
See alsoEdit
Template:Portal Template:Div col
- Gentlemen's Race (2008)
- List of Ultras of the United States
- Mount Hood climbing accidents
- Mount Hood Corridor
- Mount Hood Railroad
ReferencesEdit
External linksEdit
- "Mount Hood". The Oregon Encyclopedia
- {{#invoke:citation/CS1|citation
|CitationClass=web }}
- "Mount Hood: Climbing Oregon's Highest Peak". Oregon Field Guide.
- "Mt. Hood's Volcanic Past". Oregon Field Guide.
Template:US prominent Template:U.S. State Highest Points Template:Cascade volcanoes Template:Volcanoes of Oregon Template:Glaciers of Mount Hood Template:Authority control Template:Portal bar