- Mount Hood
Mount Hood reflected in Mirror Lake
Elevation 11,249 ft (3,429 m) NAVD 88 Prominence 7,706 ft (2,349 m)  Listing Ultra
U.S. state high point
Location Clackamas / Hood River counties, Oregon, USA Range Cascade Range Coordinates Coordinates:  Topo map USGS Mount Hood South Geology Type Stratovolcano Age of rock More than 500,000 years Volcanic arc/belt Cascade Volcanic Arc Last eruption 1866 Climbing First ascent 1857-07-11 by Henry Pittock, W. Lymen Chittenden, Wilbur Cornell, and the Rev. T.A. Wood Easiest route Rock and glacier climb
Mount Hood, called Wy'east by the Multnomah tribe, is a stratovolcano in the Cascade Volcanic Arc of northern Oregon. It was formed by a subduction zone and rests in the Pacific Northwest region of the United States. It is located about 50 miles (80 km) east-southeast of Portland, on the border between Clackamas and Hood River counties.
The height assigned to Mount Hood's snow-covered peak has varied over its history. Modern sources point to three different heights: 11,249 feet (3,429 m) based on the 1991 U.S. National Geodetic Survey, 11,240 feet (3,426 m) based on a 1993 scientific expedition, and 11,239 feet (3,426 m) of slightly older origin. The peak is home to twelve glaciers. It is the highest point in Oregon and the fourth-highest in the Cascade Range. Mount Hood is considered the Oregon volcano most likely to erupt, though based on its history, an explosive eruption is unlikely. Still, the odds of an eruption in the next 30 years are estimated at between 3 and 7 percent, so the USGS characterizes it as "potentially active", but the mountain is informally considered dormant.
The mountain has six ski areas: Timberline, Mount Hood Meadows, Ski Bowl, Cooper Spur, Snow Bunny, and Summit. They total over 4,600 acres (7.2 sq mi; 18.6 km2) of skiable terrain; Timberline offers the only year-round lift-served skiing in North America.
Mount Hood is part of the Mount Hood National Forest, which has 1.067 million acres (1667 sq mi/4318 km²), four designated wilderness areas which total 189,200 acres (295.6 sq mi; 766 km2) and more than 1,200 miles (1,900 km) of hiking trails.
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.
The last three 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 last eruptive period took place around 170 to 220 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 1781–82 with a slightly more recent episode ending shortly before the arrival of Lewis and Clark in 1805. The latest minor eruptive event occurred in August 1907.
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 noxious gases such as carbon dioxide and sulfur dioxide. 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.
Since 1950, there have been several earthquake swarms each year at Mount Hood, most notably in July 1980 and June 2002. Seismic activity is monitored by the USGS Cascades Volcano Observatory located in Vancouver, Washington, which issues weekly updates (or daily updates when significant eruptive activity is occurring at a Cascades volcano).
Since first seen by European explorers in 1792, Mount Hood 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.
Date Elevation By 1854 18,361 ft (5,596 m) Thomas J. Dryer 1854 19,400 ft (5,900 m) Belden  1857 14,000 ft (4,300 m) Mitchell's School Atlas  1866 17,600 ft (5,400 m) Rev. Atkinson  1867 11,225 ft (3,421 m) Col. Williamson  1916 11,253 ft (3,430 m) Adm. Colbert  1939 11,245 ft (3,427 m) Adm. Colbert  1980 11,239 ft (3,426 m) USGS using NGVD 29  1991 11,249 ft (3,429 m) NGS using NAVD 88  1993 11,240 ft (3,430 m) scientific expedition and 11,239 feet (3,426 m) of slightly older origin. 2008? 11,235 ft (3,424 m) Encyclopædia Britannica 
Early explorers on the Columbia River estimated the elevation to be 10,000 to 12,000 feet (3,000 to 3,700 m). Two persons in Thomas J. Dryer's 1854 expedition calculated the elevation to be 18,361 feet (5,596 m) and that the tree line was at about 11,250 feet (3,430 m). Two months later, a Mr. Belden claimed to have climbed the mountain during a hunting trip and determined it to be 19,400 feet (5,900 m) upon which "pores oozed blood, eyes bled, and blood rushed from their ears." Sometime by 1866, Reverend G. H. Atkinson determined it to be 17,600 feet (5,400 m). A Portland engineer used surveying methods from a Portland baseline and calculated a height of between 18,000 and 19,000 feet (5,500 and 5,800 m). Many maps distributed in the late 19th century cited 18,361 feet (5,596 m), though Mitchell's School Atlas gave 14,000 feet (4,300 m) as the correct value. For some time, many references assumed Mount Hood to be the highest point in North America.
Modern height surveys also vary but not by the huge margins seen in the past. A 1993 survey by a scientific party who arrived at the peaks summit carrying 16 pounds of electronic equipment reported a height of 11,240 feet (3425.952 m), claimed to be accurate to within 1.25 inches (32 mm). Many modern sources likewise list 11,240 feet (3,430 m) as the height. However, numerous others place the peak's height one foot lower, at 11,239 feet (3,426 m). Finally, a height of 11,249 feet (3,429 m) has also been reported.
Mount Hood's treeline varies from about 5,500 feet (1,700 m), mostly on the western faces, to about 7,000 feet (2,100 m), mostly on the eastern side.
Mount Hood is host to twelve 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 6,000-foot (1,800 m) level, which also is about the average tree line elevation on Mount Hood. More than 80% of the glacial surface area is above 7,000 feet (2,100 m).
The glaciers and permanent snow fields have an area of 3,331 acres (13.48 km2) and contain a volume of about 282,000 acre feet (0.348 km3). Eliot Glacier is the largest glacier by volume at 73,000 acre feet (0.090 km3), and has the thickest depth measured by ice radar at 361 feet (110 m). The largest glacier by surface area is the Coe-Ladd Glacier system at 531 acres (2.15 km2).
Glaciers and snowfields cover about 80 percent of the mountain above the 6,900-foot (2,100 m) level. The glaciers have lost an average of 34% over the 20th century (1907–2004). 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. The neo-glacial maximum extents formed in the early 18th century.
During the last major glacial event between 10,000 and 29,000 years ago, glaciers reached down to the 2,300-foot (700 m) to 2,600-foot (790 m) level: a distance of 9.3 miles (15.0 km) from the summit. The retreat released considerable outwash, some of which filled and flattened the upper Hood River Valley near Parkdale and also formed Dee Flat.
The Multnomah name for Mount Hood is Wy'east. In one version of the legend 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 Klickitat, 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 Klickitat. 
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.
The mountain was given its present name on October 29, 1792 by Lt. William Broughton, a member of Captain George Vancouver's discovery 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 a British admiral, Samuel Hood.
Lewis and Clark were the first Americans of European descent to see 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 37 miles (60 km). 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.
Two French explorers from 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.
Mount Hood is Oregon's highest point and a prominent landmark visible up to a hundred miles away. It has convenient access and minimum of technical climbing challenges. About 10,000 people attempt to climb Mount Hood each year.
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. Climbers then proceed around Crater Rock and cross Coalman glacier on the Hogsback, a ridge spanning from Crater Rock to the approach to the summit. The Hogsback terminates at a bergschrund where Coalman glacier separates from the summit rock headwall, and then to the Pearly Gates, a gap in the summit rock formation. Once through the Pearly Gates, climbers proceed to the right onto the summit plateau and then to the summit proper.
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 is recommending several other route options due to these changes in conditions (e.g. "Old Chute", West Crater Rim, etc.).
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. 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. Despite a quadrupling of forest visitors since 1990, fewer than 50 people require rescue per year. Only 3.4 percent of search and rescue missions in 2006 were for mountain climbers.
The Timberline Trail, which circumnavigates the entire mountain, was built in the 1930s by the Civilian Conservation Corps. Typically, the 40.7-mile (65.5 km) hike is snow-free from late July until the autumn snows begin. A portion of the Pacific Crest Trail is coincident with the Timberline Trail on the west side of Mount Hood.
There have been two US Navy ammunition ships named for the mountain. 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. A second ammunition ship, AE-29, was commissioned in May 1971 and decommissioned in August 1999.
- Cascade Volcanoes
- Barlow Road, pioneer road over the south flank built in 1846
- Mount Hood Corridor
- Mount Hood Railroad
- Mountain peaks of North America
- Mountain peaks of the United States
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- "Mt. Hood History". mounthoodhistory.com. http://www.mounthoodhistory.com/. Retrieved 2008-12-19.
- Aerial photos at HHood.
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