Mount McKinley | |
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Mount McKinley (also known as Denali) from Denali National Park |
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Mount McKinley
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Elevation | 6,193.6 metres (20,320 ft)[1] |
Location | Denali National Park and Preserve, Alaska, USA |
Range | Alaska Range |
Prominence | 6,138 metres (20,138 ft) Ranked 3rd |
Coordinates | |
Topo map | USGS Mt. McKinley A-3 |
First ascent | June 7, 1913 Hudson Stuck Harry Karstens Walter Harper Robert Tatum |
Easiest route | West Buttress Route (glacier/snow climb) |
Listing | Seven summits Country high point Ultra U.S. state high point |
Mount McKinley or Denali ("The Great One") in Alaska is the highest mountain peak in North America, at a height of approximately 20,320 feet (6,194 m).[1] It is the centerpiece of Denali National Park.
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Mount McKinley has a larger bulk and rise than Mount Everest. Even though the summit of Everest is about 9,000 feet (2,700 m) higher as measured from sea level, its base sits on the Tibetan Plateau at about 17,000 feet (5,200 m), giving it a real vertical rise of a little more than 12,000 feet (3,700 m). The base of Mount McKinley is roughly a 2,000-foot plateau, giving it an actual rise of 18,000 feet (5,500 m).
The mountain is also characterized by extremely cold weather. A thermometer left exposed at an elevation of 15,000 feet (4,600 m) on Mount McKinley over 19 years recorded a temperature of −100 °F (−73.3 °C) at some point during its exposure . There is also a higher risk of altitude illness for climbers than its altitude would otherwise suggest, due to its high latitude.[2] At the equator, a mountain as high as Mount McKinley would have 47% as much oxygen available on its summit as there is at sea level,[3] but because of its latitude, the pressure on the summit of McKinley is even lower (42%).[4]
Mount McKinley is a granitic pluton with a crystallization age of around 56 million years. Over tens of millions of years, Mount McKinley has been uplifted by tectonic pressure while at the same time, erosion has stripped away the (somewhat softer) sedimentary rock above and around it.
The forces that lifted Mount McKinley—the subduction of the Pacific plate beneath the North American plate—also raised great ranges across southern Alaska. As that huge sheet of ocean-floor rock plunges downward into the mantle, it shoves and crumples the continent into soaring mountains which include some of the most active volcanoes on the continent.
Mount McKinley has two significant summits: the South Summit is the higher one, while the North Summit has an elevation of 19,470 feet (5,934 m) and a prominence of approximately 1,320 feet (402 m). The North Summit is sometimes counted as a separate peak (see e.g., the List of United States fourteeners) and sometimes not; it is rarely climbed, except by those doing routes on the north side of the massif.
Five large glaciers flow off the slopes of the mountain. The Peters Glacier lies on the northwest side of the massif, while the Muldrow Glacier falls from its northeast slopes. Just to the east of the Muldrow, and abutting the eastern side of the massif, is the Traleika Glacier. The Ruth Glacier lies to the southeast of the mountain, and the Kahiltna Glacier leads up to the southwest side of the mountain.
Numerous native peoples of the area had their own names for this prominent peak. The local Athabaskan name for the mountain, the one used by the Native Americans with access to the flanks of the mountain (living in the Yukon, Tanana and Kuskokwim basins) is Dinale or Denali (“the Great One”). To the South the Dena’ina people in the Susitna river valley used the name Dghelay Ka’a (simplified to Doleika), meaning “the big mountain”, while the Aleuts called it Traleika.[5]
The historical first European sighting of Mount McKinley took place on May 6, 1794, when George Vancouver was surveying the Knik Arm of the Cook Inlet and mentioned “distant stupendous mountains” in his journal. However, he uncharacteristically left the mountain unnamed. The mountain is first named on a map by Ferdinand von Wrangell in 1839; the names Tschigmit and Tenada correspond to the locations of Mount Foraker and Mount McKinley. Von Wrangel had been chief administrator of the Russian settlements in North America from 1829-1835. The Russian explorer Lavrenty Zagoskin explored the Tanana and Kuskokwim rivers in 1843 and 1844 and was probably the first European to sight the mountain from the other site.[5]
The first English name the peak enjoyed, locally, was Densmore’s Mountain, after the gold prospector Frank Densmore who in 1889 had fervently praised the mountain’s majesty. The mountain did not get much press until William Dickey, a New Hampshire-born Seattleite, who had been digging for gold in the sands of the Susitna River, wrote, after his return to the lower states, an account in the New York Sun that appeared on January 24, 1897. He wrote “We named our great peak Mount McKinley, after William McKinley of Ohio, who had been nominated for the Presidency”. By most accounts, the naming was a pure political one; he had met many silver miners who zealously promoted Democratic presidential candidate William Jennings Bryan's ideal of a silver standard, inspiring him to retaliate by naming the mountain after a strong proponent of the gold standard. His report drew attention with the sentence “We have no doubt that this peak is the highest in North America, and estimate that it is over 20,000 feet (6,100 m) high.” Until then 18,000-foot (5,500 m) Mount Saint Elias was believed to be the continent’s highest (Mount Logan was still unknown, while Mount St Elias’ height had been overestimated to beat Pico de Orizaba). Though later praised for his estimate, Dickey admitted that other prospector parties had also guessed the mountain to be over 20,000 feet (6,100 m).[6]
Mount McKinley is commonly referred to by its Athabaskan name Denali, which is the name currently recognized by the State of Alaska. When Denali National Park and Preserve was established by the Alaska National Interest Lands Conservation Act, December 2, 1980, the Alaska Board of Geographic Names changed the name of the mountain back to Denali. However, the U.S. Board on Geographic Names maintains the name McKinley, ostensibly to help visitors avoid confusion between the mountain and the park. Use of the name "McKinley" remains common, particularly in the Lower 48; however, Alaskans and mountaineers generally use the name "Denali" to refer both to the park and to the mountain.[7]
The first recorded attempt to climb Mount McKinley was by Judge James Wickersham in 1903, via the Peters Glacier and the North Face, now known as the Wickersham Wall. This route has tremendous avalanche danger and was not successfully climbed until 1963.
Famed explorer Dr. Frederick Cook claimed the first ascent of the mountain in 1906. His claim was regarded with some suspicion from the start, but was also widely believed. It was later proved fraudulent, with some crucial evidence provided by Bradford Washburn when he was sketched on a lower peak.
In 1910, four locals (Tom Lloyd, Peter Anderson, Billy Taylor, and Charles McGonagall), known as the Sourdough expedition, attempted McKinley, despite a complete lack of climbing experience. They spent approximately three months on the mountain. However, their purported summit day was impressive: carrying a bag of doughnuts, a thermos of cocoa each and a 14-foot (4.2 m) spruce pole, two of them reached the North Summit, lower of the two, and erected the pole near the top. According to them, they took a total of 18 hours — a record that has yet to be breached (as of 2006). No one believed their success (partly due to false claims that they had climbed both summits) until the true first ascent, in 1913.
In 1912, the Parker-Browne expedition nearly reached the summit, turning back within just a few hundred yards of it due to harsh weather. In fact, that probably saved their lives, as a powerful earthquake shattered the glacier they ascended hours after they safely left it.
The first ascent of the main summit of McKinley came on June 7, 1913 by a party led by Hudson Stuck. The first man to reach the summit was Walter Harper, an Alaska Native. Harry Karstens and Robert Tatum also made the summit. Tatum later commented, "The view from the top of Mount McKinley is like looking out the windows of Heaven!"[8] They ascended the Muldrow Glacier route pioneered by the earlier expeditions, which is still often climbed today. Stuck confirmed, via binoculars, the presence of a large pole near the North Summit; this report confirmed the Sourdough ascent, and today it is widely believed that the Sourdoughs did succeed on the North Summit. However, the pole was never seen before or since, so there is still some doubt. Stuck also discovered that the Parker-Browne party were only about 200 feet (61 m) of elevation short of the true summit when they turned back.
See the timeline below for more important events in Mount McKinley's climbing history.
The mountain is regularly climbed today, with just over 50% of the expeditions successful, although it is still a dangerous undertaking. By 2003, the mountain had claimed the lives of nearly 100 mountaineers.[9] The vast majority of climbers use the West Buttress Route, pioneered in 1951 by Bradford Washburn, after an extensive aerial photographic analysis of the mountain. Climbers typically take two to four weeks to ascend the mountain.
The Japan Alpine Club installed a meteorological station on a ridge near the summit of Denali at an altitude of 5710 m in 1990. In 1998, this weather station was donated to the International Arctic Research Center at the University of Alaska Fairbanks. In June 2002, a weather station was placed at the 19,000-foot (5,800 m) level. This weather station was designed to transmit data in real-time for use by the climbing public and the science community. Since its establishment, annual upgrades to the equipment have been performed with instrumentation custom built for the extreme weather and altitude conditions. This weather station is one of only two weather stations in the world located above 18,000 feet (5,500 m).
Besides the North Summit mentioned above, other less significant features on the massif which are sometimes included as separate peaks are:
None of these peaks is usually regarded as worthwhile objectives in their own right; however they often appear on lists of the highest peaks of the United States. (Only one appears on the List of United States Fourteeners on Wikipedia.)
Nearby important peaks include:
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