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Denali
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Denali (/dəˈnɑːli/),[5] federally designated as Mount McKinley,[6][7] is the highest mountain peak in North America, with a summit elevation of 20,310 feet (6,190 m) above sea level. It is the tallest mountain in the world from base to peak on land, measuring 18,000 ft (5,500 m).[8] With a topographic prominence of 20,156 feet (6,144 m)[3] and a topographic isolation of 4,621.1 miles (7,436.9 km),[3] Denali is the third most prominent and third-most isolated peak on Earth, after Mount Everest and Aconcagua. Located in the Alaska Range in the interior of the U.S. state of Alaska, Denali is the centerpiece of Denali National Park and Preserve.
Key Information
The Koyukon people who inhabit the area around the mountain have referred to the peak as "Denali" for centuries. In 1896, a gold prospector named it "Mount McKinley" in support of then-presidential candidate William McKinley, who later became the 25th president; McKinley's name was the official name recognized by the federal government of the United States from 1917 until 2015. In August 2015, 40 years after Alaska had officially named the mountain Denali, the United States Department of the Interior under the Obama administration changed the official federal name of the mountain also to Denali.[9][10][11] In January 2025, the Department of the Interior under the Trump administration reverted the mountain's official federal name to Mount McKinley.[12][6]
In 1903, James Wickersham recorded the first attempt at climbing Denali, which was unsuccessful. In 1906, Frederick Cook claimed the first ascent, but this ascent is unverified and its legitimacy questioned. The first verifiable ascent to Denali's summit was achieved on June 7, 1913, by climbers Hudson Stuck, Harry Karstens, Walter Harper, and Robert Tatum, who went by the South Summit. In 1951, Bradford Washburn pioneered the West Buttress route, considered to be the safest and easiest route, and therefore the most popular currently in use.[13]
On September 2, 2015, the U.S. Geological Survey measured the mountain at 20,310 feet (6,190 m) high,[1] 10 ft lower than the 20,320 feet (6,194 m) measured in 1952 using photogrammetry.
Geology and features
[edit]Denali is a granitic pluton, mostly pink quartz monzonite, lifted by tectonic pressure from the subduction of the Pacific Plate beneath the North American Plate; at the same time, the sedimentary material above and around the mountain was stripped away by erosion.[14][15] The forces that lifted Denali also caused many deep earthquakes in Alaska and the Aleutian Islands. The Pacific Plate is seismically active beneath Denali, a tectonic region that is known as the "McKinley cluster".[16]
Structural geology
[edit]The high topography of Denali is related to the complex structural relationships created by the right-lateral Denali Fault and Denali Fault Bend. The Denali Fault is caused by stresses created by the low-angle subduction of the Yakutat microplate underneath Alaska. The Denali Fault Bend is characterized as a gentle restraining bend.[17] The Denali Fault Bend represents a curvature in the Denali Fault that is approximately 75 km long. This curvature creates what is known as a "space problem". As the right-lateral movement along the Denali Fault continues, high compressional forces created at the fault bend essentially push the crust up in a vertical fashion. The longer the crust stays within the restraining bend, the higher the topography will be. Several active normal faults north of the restraining bend have recently been mapped with slip rates of approximately 2–6 mm/year.[17] These normal faults help to accommodate the unusual curvature of the restraining bend.[citation needed]
Elevation
[edit]Denali has a summit elevation of 20,310 feet (6,190 m) above sea level, making it the highest peak in North America and the northernmost mountain above 19,685 feet (6,000 m) elevation in the world.[1] Measured from base to peak at some 18,000 ft (5,500 m), it is among the largest mountains situated entirely above sea level. Denali rises from a sloping plain with elevations from 1,000 to 3,000 ft (300 to 910 m), for a base-to-peak height of 17,000 to 19,000 ft (5,000 to 6,000 m).[18] By comparison, Mount Everest rises from the Tibetan Plateau at a much higher base elevation. Base elevations for Everest range from 13,800 ft (4,200 m) on the south side to 17,100 ft (5,200 m) on the Tibetan Plateau, for a base-to-peak height in the range of 12,000 to 15,300 ft (3,700 to 4,700 m).[19] Denali's base-to-peak height is little more than half the 33,500 ft (10,200 m) of the volcano Mauna Kea, which lies mostly under water.[20]
Geography of the mountain
[edit]Denali has two significant summits: the South Summit is the higher one, while the North Summit has an elevation of 19,470 ft (5,934 m)[14] and a prominence of approximately 1,270 ft (387 m).[21] The North Summit is sometimes counted as a separate peak (see e.g., fourteener) 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.[22][23] With a length of 44 mi (71 km), the Kahiltna Glacier is the longest glacier in the Alaska Range.
Naming
[edit]The Koyukon Athabaskans who inhabit the area around the mountain have, for centuries, referred to the peak as Dinale or Denali. The name is based on a Koyukon word for 'high' or 'tall'.[24] During the Russian ownership of Alaska, the common name for the mountain was Bolshaya Gora (Russian: Большая Гора; bolshaya 'big'; gora 'mountain'), which is the Russian translation of Denali.[25] It was briefly called Densmore's Mountain in the late 1880s and early 1890s[26] after Frank Densmore, a gold prospector who was the first non-native Alaskan to reach the base of the mountain.[27]
William A Dickey
[edit]In 1896, gold prospector William Dickey[28][29] named it McKinley as political support for then-presidential candidate William McKinley, who became president the following year.
One, however, W. A. Dickey, of a different type from the rest, recognized the surpassing height of the peak and its geographic import and gave it the name Mount McKinley. His exploration in 1896 was probably one of the first extensive journeys in this district since that of the Russian Malakoff in 1834. With three other men he ascended Susitna River to the trading station at the head of the delta; then constructed boats of whipsawed lumber and continued his journey up the main Susitna to the mouth of Indian Creek. From this place he explored a part of the upper canyon of the Susitna and also made a journey westward to the Chulitna, reaching the foot of the glacier which discharges into this river and has its source on the slopes of Mount McKinley. It was after this journey that he published his description of the mountain, in which he named it and stated its altitude as over 20,000 feet. He told the writer that he had no instruments, but made his estimate, which has proved to be remarkably accurate, with careful consideration of the atmospheric conditions, as well as of the probable distance to the base of the peak. In 1897 he made a second trip into this region, with one companion, and extended his previous explorations. He was the first to call attention to the great lowland drained by Tokichitna River and to the low divide which separates it from the Kuskokwim drainage, later explored by Spurr, Herron, and the writer.
— Alfred H Brooks, "The Mount McKinley Region, Alaska", Department of the Interior, United States Geological Survey, Professional Paper 70[29]
The United States formally recognized the name Mount McKinley after President Woodrow Wilson signed the Mount McKinley National Park Act of February 26, 1917.[30] In 1965, President Lyndon B. Johnson declared the north and south peaks of the mountain the "Churchill Peaks", in honor of British statesman Winston Churchill.[31] The Alaska Board of Geographic Names changed the state name of the mountain to Denali in 1975, which was how it was referred to locally.[11][32] However, a request in 1975 from the Alaska state legislature to the United States Board on Geographic Names to do the same at the federal level was blocked by Ohio congressman Ralph Regula, whose district included McKinley's home town of Canton.[33]
On August 28, 2015, just ahead of a presidential visit to Alaska, the Barack Obama administration changed the mountain's official federal name to Denali,[9] bringing it in line with the Alaska Geographic Board's designation.[10][34] U.S. Secretary of the Interior Sally Jewell said the change had been "a long time coming".[35] The renaming of the mountain received praise from Alaska's senior U.S. senator, Republican Lisa Murkowski,[36] who had previously introduced legislation to accomplish the name change,[37] but it drew criticism from several politicians from President McKinley's home state of Ohio, such as Governor John Kasich, U.S. Senator Rob Portman, U.S. House Speaker John Boehner, and Representative Bob Gibbs, who described Obama's action as "constitutional overreach" because he said an act of Congress was required to rename the mountain.[38][39][40] The Alaska Dispatch News reported that the secretary of the interior has authority under federal law to change geographic names when the Board of Geographic Names does not act on a naming request within a "reasonable" period of time. Jewell told the Alaska Dispatch News that "I think any of us would think that 40 years is an unreasonable amount of time."[24]
In December 2024, President-elect Donald Trump stated that he planned to revert the mountain's official federal name back to Mount McKinley during his second term, in honor of President William McKinley. Trump had previously proposed changing the name in 2017, drawing opposition from Alaska's Republican governor Mike Dunleavy.[41] His 2017 proposal was strongly opposed by both Republican U.S. senators from Alaska, Murkowski and Dan Sullivan,[42] who, along with Alaska State Senator Scott Kawasaki, a Democrat, again expressed their preference for Denali in 2024.[43] On January 20, 2025, shortly after his second inauguration, Trump signed an executive order requiring the secretary of the interior to revert the Obama-era name change within 30 days of signing, renaming Denali back to Mount McKinley in official maps and communications from the American federal government.[44] The executive order does not change the name of Denali National Park.[45] On January 23, 2025, the Department of the Interior changed the mountain's official federal name back to Mount McKinley.[12][6] The same day, the Associated Press announced that it would use Mount McKinley instead of Denali, with the reasoning that as president, Trump has the authority to change federal geographical names of features lying within national borders.[46]
Hudson Stuck, the organizer of the Stuck-Karstens Expedition, which was the first confirmed team to summit the mountain, preferred the name Denali over McKinley, referring to it as Denali nearly exclusively in his account of the expedition.[47]
According to the Alaska Department of Commerce, Community, and Economic Development's official database of business licenses, businesses named after Denali outnumber those named after McKinley by a margin of six to one.[48]
Indigenous names for Denali can be found in seven different Alaskan languages. The names fall into two categories. To the south of the Alaska Range in the Dena'ina and Ahtna languages the mountain is known by names that are translated as 'big mountain'. To the north of the Alaska Range in the Lower Tanana, Koyukon, Upper Kuskokwim, Holikachuk, and Deg Xinag languages the mountain is known by names that are translated as 'the high one',[49] 'the tall one' (Koyukon, Lower and Middle Tanana, Upper Kuskokwim, Deg Xinag, and Holikachuk).[50]
Asked about the importance of the mountain and its name, Will Mayo, former president of the Tanana Chiefs Conference, an organization that represents 42 Athabaskan tribes in the Alaskan interior, said: "It's not one homogeneous belief structure around the mountain, but we all agree that we're all deeply gratified by the acknowledgment of the importance of Denali to Alaska's people."[51]
The following table lists the Alaskan Athabascan names for Denali.[50]
| Literal meaning | Native language | Spelling in the local practical alphabet |
Spelling in a standardized alphabet |
IPA transcription |
|---|---|---|---|---|
| 'The tall one' | Koyukon | Deenaalee | Diinaalii | /diːˈnæli/ |
| Lower Tanana | Deenadheet, Deenadhee | Diinaadhiit, Diinaadhii | /diˈnæðid/ | |
| Middle Tanana | Diineezi | Diinaadhi | /diˈnæði/ | |
| Upper Kuskokwim | Denaze | Diinaazii | /diˈnæzi/ | |
| Deg Xinag | Dengadh, Dengadhi | Dengadh, Dengadhe | /təˈŋað, təˈŋaðə/ | |
| Holikachuk | Denadhe | Diinaadhii | /diːˈnæðiː/ | |
| 'Big mountain' | Ahtna | Dghelaay Ce'e, Deghilaay Ce'e | Dghelaay Ke'e, Deghilaay Ke'e | /dʁɛˈlɔj ˈkɛʔɛ/ |
| Upper Inlet Dena'ina | Dghelay Ka'a | Dghelay Ka'a | /dʁəˈlaj ˈkaʔa/ | |
| Lower Inlet Dena'ina | Dghili Ka'a | Dghili Ka'a | /dʁili ˈkaʔa/ |
History
[edit]
The Koyukon Athabaskans, living in the Yukon, Tanana and Kuskokwim basins, were the first Native Americans with access to the flanks of the mountain.[4] A British naval captain and explorer, George Vancouver, is the first European on record to have sighted Denali, when he noted "distant stupendous mountains" while surveying the Knik Arm of the Cook Inlet on May 6, 1794.[52] The Russian explorer Lavrenty Zagoskin explored the Tanana and Kuskokwim rivers in 1843 and 1844, and was likely the first European to sight the mountain from the other side.[53]
William Dickey, a New Hampshire-born resident of Seattle, Washington, who had been digging for gold in the sands of the Susitna River, wrote, after his returning from Alaska, an account in the New York Sun that appeared on January 24, 1897.[54] 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, Mount Logan in Canada's Yukon Territory was believed to be the continent's highest point. 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).[55] These estimates were confirmed in 1898 by the surveyor Robert Muldrow, who measured its elevation as 20,300 feet (6,200 m).[56]
On November 5, 2012, the United States Mint released a twenty-five cent piece depicting Denali National Park. It is the fifteenth of the America the Beautiful Quarters series. The reverse features a Dall sheep with the peak of Denali in the background.[57]
Climbing history
[edit]During the summer of 1902 scientist Alfred Brooks explored the flanks of the mountain as a part of an exploratory surveying party conducted by the U.S. Geological Survey. The party landed at Cook Inlet in late May, then traveled east, paralleling the Alaska Range, before reaching the slopes of Denali in early August. Camped on the flank of the mountain on August 3, Brooks noted later that while "the ascent of Mount McKinley had never been part of our plans", the party decided to delay one day so "that we might actually set foot on the slopes of the mountain". Setting off alone, with good weather, on August 4, Brooks aimed to reach a 10,000 feet (3,048 m) shoulder. At 7,500 feet (2,286 m), Brooks found his way blocked by sheer ice and, after leaving a small cairn as a marker, descended.[58] After the party's return, Brooks co-authored a "Plan For Climbing Mt McKinley", published in National Geographic magazine in January 1903, with fellow party-member and topographer D. L. Raeburn, in which they suggested that future attempts at the summit should approach from the north, not the south.[59] The report received substantial attention, and within a year, two climbing parties declared their intent to summit.[60]
During the early summer of 1903, Judge James Wickersham, then of Eagle, Alaska, made the first recorded attempt to climb Denali, along with a party of four others. The group attempted to get as close to the mountain as possible via the Kantishna river by steamer, before offloading and following Chitsia Creek with a poling boat, mules and backpacks, a route suggested to them by Tanana Athabaskan people they met along the way. The party received further navigational assistance at Anotoktilon, an Athabaskan hunting camp, where residents gave the group detailed directions to reach the glaciers at the foot of Denali. On reaching the mountain, the mountaineers set up base camp on the lower portion of Peters Glacier. Aiming for the northwest buttress of Denali's north peak, they attempted to ascend directly; however, crevasses, ice fall and the lack of a clear passage caused them to turn and attempt to follow a spur via Jeffery Glacier where they believed they could see a way to the summit. After a dangerous ascent, at around 10,000 feet (3,048 m), Wickersham found that the route did not connect as it had appeared from below, instead discovering "a tremendous precipice beyond which we cannot go. Our only line of further ascent would be to climb the vertical wall of the mountain at our left, and that is impossible." This wall, now known as the Wickersham Wall, juts 15,000 feet (4,572 m) upwards from the glacier to the north peak of Denali.[61] Because of the route's history of avalanche danger, it was not successfully climbed until 1963.[62]
Later in the summer of 1903, Dr. Frederick Cook directed a team of five men on another attempt at the summit. Cook was already an experienced explorer and had been a party-member on successful arctic expeditions commanded both by Robert Peary and Roald Amundsen.[61][63] Yet he struggled to obtain funding for his own expedition, eventually organizing it "on a shoestring budget"[64] without any other experienced climbers.[63] The party navigated up the Cook inlet and followed the path of the 1902 Brooks party towards Denali. Cook approached the mountain via the Peters Glacier, as Wickersham had done; however, he was able to overcome the ice fall that had caused the previous group to turn up the spur towards the Wickersham Wall. Despite avoiding this obstacle, on August 31, having reached an elevation of about 10,900 feet (3,322 m) on the northwest buttress of the north peak, the party found they had reached a dead end and could make no further progress. On the descent, the group completely circumnavigated the mountain, the first climbing party to do so.[65] Although Cook's 1903 expedition did not reach the summit, he received acclaim for the accomplishment – a 1,000-mile (1,609 km) trek in which he not only circled the entire mountain but also found, on the descent, an accessible pass northeast of the Muldrow Glacier following the headwaters of the Toklat and Chulitna rivers.[61]
In 1906, Cook initiated another expedition to Denali with co-leader Herschel Parker, a Columbia University professor of electrical engineering with extensive mountaineering experience. Belmore Browne, an experienced climber and five other men comprised the rest of the group. Cook and Parker's group spent most of the summer season exploring the southern and southeastern approaches to the mountain, eventually reaching a high point on Tokositna glacier, 25 miles (40 km) from the summit.[65] During their explorations the party mapped out many of the tributaries and glaciers of the Susitna river along the mountain's south flank.[61] As the summer ended, the team retreated to the coast and began to disperse. In September 1906, Cook and a single party-member, horseman Robert Barrill, journeyed towards the summit again, in what Cook later described as "a last desperate attempt" in a telegram to his financial backers.[61] Cook and Barrill spent 12 days in total on the attempt, and claimed to have reached the summit via the Ruth Glacier.[64]
Upon hearing Cook's claims, Parker and Browne were immediately suspicious. Browne later wrote that he knew Cook's claims were lies, just as "any New Yorker would know that no man could walk from the Brooklyn Bridge to Grant's Tomb [a distance of eight miles] in ten minutes."[64] In May 1907, Harper's Magazine published Cook's account of the climb along with a photograph of what appeared to be Barrill standing on the summit. By 1909, Barrill had recanted at least part of his story about the climb, and others publicly questioned the account; however, Cook continued to assert his claim.[66] The controversy continued for decades. In 1956, mountaineers Bradford Washburn and Walter Gonnason tried to settle the matter, with Gonnason attempting to follow Cook's purported route to the summit. Washburn noted inconsistencies between Cook's account of locations of glaciers and found a spot, at 5,400 feet (1,646 m) and 19 miles (31 km) southeast of the summit that appeared identical to the supposed summit image. Gonnason was not able to complete the climb, but because he was turned back by poor weather, felt that this did not definitely disprove Cook's story.[67] In 1998, historian Robert Bryce discovered an original and un-cropped version of the "fake peak" photograph of Barrill standing on the promontory. It showed a wider view of surrounding features, appearing to definitively discount Cook's claim.[68]

Given the skepticism concerning Cook's story, interest in claiming the first ascent remained. Miners and other Alaskans living in Kantishna and Fairbanks wanted the honors to go to local men. In 1909, four Alaska residents – Tom Lloyd, Peter Anderson, Billy Taylor, and Charles McGonagall – set out from Fairbanks, Alaska during late December with supplies and dogs that were in part paid for by bettors in a Fairbanks tavern. By March 1910, the men had established a base camp near one of the sites where the Brooks party had been and pressed on from the north via the Muldrow glacier. Unlike some previous expeditions, they discovered a pass, since named McGonagall Pass, which allowed them to bypass the Wickersham Wall and access the higher reaches of the mountain. At roughly 11,000 feet (3,353 m), Tom Lloyd, old and less physically fit than the others, stayed behind. According to their account, the remaining three men pioneered a route following Karstens Ridge around the Harper Icefall, then reached the upper basin before ascending to Pioneer Ridge. The three men carried a 14-foot-long (4.3 m) spruce pole. Around 19,000 feet (5,791 m), Charles McGonagall, older and having exhausted himself carrying the spruce pole, remained behind. On April 3, 1910, Billy Taylor and Peter Anderson scrambled the final few hundred feet to reach the north peak of Denali, at 19,470 feet (5,934 m) high, the shorter of the two peaks. The pair erected the pole near the top, with the hope that it would be visible from lower reaches to prove they had made it.[69]
After the expedition, Tom Lloyd returned to Fairbanks, while the three others remained in Kantishna to mine. In Lloyd's recounting, all four men made it to the top of not only the north peak, but the higher south peak as well. When the remaining three men returned to town with conflicting accounts, the entire expedition's legitimacy was questioned.[70] Several years later, another climbing group would claim to have seen the spruce pole in the distance, supporting their north peak claim.[69] However, some continue to doubt they reached the summit. Outside of the single later climbing group, who were friendly with some of the Sourdough expedition men, no other group would ever see it. Jon Waterman, author of the book Chasing Denali, which explored the controversy, outlined several reasons to doubt the claim: There was never any photographic evidence. The four men climbed during the winter season, known for much more difficult conditions, along a route that has never been fully replicated. They were inexperienced climbers, ascending without any of the usual safety gear or any care for altitude sickness. They claimed to have ascended from 11,000 feet (3,353 m) to the top in less than 18 hours, unheard of at a time when siege-style alpinism was the norm.[71] Yet Waterman says "these guys were men of the trail. They didn't care what anybody thought. They were just tough SOBs."[72] He noted that the men were largely unlettered and that some of the ensuing doubt was related to their lack of sophistication in dealing with the press and the contemporary climbing establishment.[71]
In 1912, the Parker-Browne expedition nearly reached the summit, turning back within just a few hundred yards/meters of it due to harsh weather. On July 7, the day after their descent, a 7.4-magnitude earthquake shattered the glacier they had ascended.[73][74][75]
The first ascent of the main summit of Denali came on June 7, 1913, by a party directed by Hudson Stuck and Harry Karstens, along with Walter Harper and Robert Tatum. Karstens relocated to Alaska in the gold rush of 1897, and in subsequent years became involved in a variety of endeavors beyond mining, including helping establish dog mushing routes to deliver mail across vast swathes of territory and supporting expeditions led by naturalist Charles Sheldon near the base of Denali.[76] Stuck was an English-born Episcopal priest who came to Alaska by chance. He became acclimated to the often harsh Alaskan environment because of his many travels between far-flung outposts within his district, climbing mountains as a hobby.[77] At 21 years old, Harper was already known as a skilled and strong outdoorsman, the Alaska-born son of a Koyukon-Athabascan mother and Irish gold prospector father.[78][79] Tatum, also 21 years old, was a theology student working at a Tanana mission, and the least experienced of the team. His primary responsibility on the trip was as a cook.[80]
The team approached the peak from the north via the Muldrow glacier and McGonagall pass. While ferrying loads up to a camp at around 10,800 feet (3,292 m), they suffered a setback when a stray match accidentally set fire to some supplies, including several tents. The prior year's earthquake had left what had previously been described by the Parker-Browne expedition as a gentle slope ascended in no more than three days as a dangerous, ice-strewn morass on a knife-edged ridge (later named Karstens ridge). It would take the team three weeks to cover the same ground, as Karstens and Harper laboriously cut steps into the ice. On May 30, the team, with the help of some good weather, ascended to a new high camp, situated at 17,500 feet (5,334 m) in the Grand Basin between the north and south peaks. On June 7, the team made the summit attempt. Temperatures were below −20 °F (−29 °C) at times. Every man, and particularly Stuck, suffered from altitude sickness. By midday, Harper became the first climber to reach the summit, followed seconds later by Tatum and Karstens. Stuck arrived last, falling unconscious on the summit.[81]
Using the mountain's contemporary name, Tatum later commented, "The view from the top of Mount McKinley is like looking out the windows of Heaven!"[82] During the climb, Stuck spotted, via binoculars, the presence of a large pole near the North Summit; this report confirmed the Sourdough ascent, and it is widely believed presently 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. Stuck and Karstens' team achieved the uncontroversial first ascent of Denali's south peak; however, the news was met with muted interest by the wider climbing community. Appalachia Journal, then the official journal of the American Alpine Club, published a small notice of the accomplishment a year later.[77]
The mountain is climbed regularly nowadays. In 2003, around 58% of climbers reached the top. But by that time, the mountain had claimed the lives of nearly 100 mountaineers.[83] The vast majority of climbers use the West Buttress Route, pioneered in 1951 by Bradford Washburn,[13] after an extensive aerial photographic analysis of the mountain. Climbers typically take two to four weeks to ascend Denali. It is one of the Seven Summits; summiting all of them is a challenge for mountaineers.
Accidents
[edit]From 1947 to 2018 in the United States "2,799 people were reported to be involved in mountaineering accidents"[84] and 11% of these accidents occurred on Denali.[84] Of these 2,799 accidents, 43% resulted in death and 8% of these deaths occurred on Denali.[84]
Timeline
[edit]

- 1896–1902: Surveys by Robert Muldrow, George Eldridge, Alfred Brooks.[85]
- 1913: First ascent, by Hudson Stuck, Harry Karstens, Walter Harper, and Robert Tatum via the Muldrow Glacier route.[86]
- 1932: Second ascent, by Alfred Lindley, Harry Liek, Grant Pearson, Erling Strom. (Both peaks were climbed.)[87][88]
- 1947: Barbara Washburn becomes the first woman to reach the summit while her husband Bradford Washburn becomes the first person to summit twice.[89]
- 1951: First ascent of the West Buttress Route, led by Bradford Washburn.[13]
- 1954: First ascent of the very long South Buttress Route by George Argus, Elton Thayer (died on descent), Morton Wood, and Les Viereck. Deteriorating conditions behind the team pushed them to make the first traverse of Denali. The Great Traleika Cirque, where they camped just below the summit, was renamed Thayer Basin, in honor of the fallen climber.[90][91]
- 1954 (May 27) First ascent via Northwest Buttress to North Peak by Fred Beckey, Donald McLean, Charles Wilson, Henry Meybohm, and Bill Hackett[92]
- 1959: First ascent of the West Rib, now a popular, mildly technical route to the summit.[90]
- 1961: First ascent of the Cassin Ridge, named for Riccardo Cassin and the best-known technical route on the mountain.[93] The first ascent team members are: Riccardo Cassin, Luigi Airoldi, Luigi Alippi, Giancarlo Canali, Romano Perego, and Annibale Zucchi.[94][95]

- 1962: First ascent of the southeast spur, team of six climbers (C. Hollister, H. Abrons, B. Everett, Jr., S. Silverstein, S. Cochrane, and C. Wren)[96]
- 1963: A team of six climbers (W. Blesser, P. Lev, R. Newcomb, A. Read, J. Williamson, F. Wright) made the first ascent of the East Buttress. The summit was attained via Thayer Basin and Karstens Ridge. See AAJ 1964.
- 1963: Two teams make first ascents of two different routes on the Wickersham Wall.[97][98]
- 1967: First winter ascent, via the West Buttress, by Gregg Blomberg, Dave Johnston, Art Davidson and Ray Genet.[99]
- 1967: The 1967 Mount McKinley disaster; Seven members of Joe Wilcox's twelve-man expedition perish, while stranded for ten days near the summit, in what has been described as the worst storm on record. Up to that time, this was the third worst disaster in mountaineering history in terms of lives lost.[100] Before July 1967 only four men had ever perished on Denali.[101]
- 1970: First solo ascent by Naomi Uemura.[102]
- 1970: First ascent by an all-female team (the "Denali Damsels"), led by Grace Hoeman and the later famous American high altitude mountaineer Arlene Blum together with Margaret Clark, Margaret Young, Faye Kerr and Dana Smith Isherwood.[103][90]
- 1972: First descent on skis down the sheer southwest face, by Sylvain Saudan, "Skier of the Impossible".[104]
- 1976: First solo ascent of the Cassin Ridge by Charlie Porter, a climb "ahead of its time".[94]
- 1979: First ascent by dog team achieved by Susan Butcher, Ray Genet, Brian Okonek, Joe Redington, Sr., and Robert Stapleton.[90]
- 1984: Uemura returns to make the first winter solo ascent, but dies after summitting.[105] Tono Križo, František Korl and Blažej Adam from the Slovak Mountaineering Association climb a very direct route to the summit, now known as the Slovak Route, on the south face of the mountain, to the right of the Cassin Ridge.[106] Sarah Doherty became the first amputee to reach the summit in August.[107][108]
- 1988: First successful winter solo ascent. Vern Tejas climbed the West Buttress alone in February and March, summitted successfully, and descended.[109]
- 1989: Japanese climbing team of Noboru Yamada, Teruo Saegusa and Kozo Komatsu died of a presumed fall and exposure while making a winter attempt via the West Buttress route.[110]
- 1990: Anatoli Boukreev climbed the West Rib in 10 hours and 30 mins from the base to the summit, at the time a record for the fastest ascent.[111]
- 1995: French skiers Jean-Noel Urban and Nicolas Bonhomme, made the first ski descent down the Wickersham Wall, most of the face was 50°.[112]
- 1997: First successful ascent up the West Fork of Traleika Glacier up to Karstens Ridge beneath Browne Tower. This path was named the "Butte Direct" by the two climbers Jim Wilson and Jim Blow.[113][114]
- 2015: On June 24, a survey team led by Blaine Horner placed two global positioning receivers on the summit to determine the precise position and elevation of the summit. The summit snow depth was measured at 15 ft (4.6 m). The United States National Geodetic Survey later determined the summit elevation to be 20,310 ft (6,190 metres).[1]
- 2019: On June 20, Karl Egloff (Swiss-Ecuadorian) set new speed records for the ascent (7h 40m) and round-trip (11h 44m), starting and returning to a base camp at 7,200 ft (2,200 m) on the Kahiltna Glacier.[115][116]
Weather station
[edit]
The Japanese Alpine Club installed a meteorological station on a ridge near the summit of Denali at an elevation of 18,733 feet (5,710 m) in 1990.[117] In 1998, this weather station was donated to the International Arctic Research Center at the University of Alaska Fairbanks.[117] 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 the third-highest weather station in the world.[118]
The weather station recorded a temperature of −75.5 °F (−59.7 °C) on December 1, 2003. On the previous day of November 30, 2003, a temperature of −74.4 °F (−59.1 °C) combined with a wind speed of 18.4 miles per hour (29.6 km/h) to produce a North American record windchill of −118.1 °F (−83.4 °C).
Even in July, this weather station has recorded temperatures as low as −22.9 °F (−30.5 °C) and windchills as low as −59.2 °F (−50.7 °C).
Historical record
[edit]According to the National Park Service, in 1932 the Liek-Lindley expedition recovered a self-recording minimum thermometer left near Browne's Tower, at about 15,000 feet (4,600 m), on Denali by the Stuck-Karstens party in 1913. The spirit thermometer was calibrated down to −95 °F (−71 °C), and the lowest recorded temperature was below that point. Harry J. Liek took the thermometer back to Washington, D.C. where it was tested by the United States Weather Bureau and found to be accurate. The lowest temperature that it had recorded was found to be approximately −100 °F (−73 °C).[119] Another thermometer was placed at the 15,000-foot (4,600 m) level by the U.S. Army Natick Laboratory, and was there from 1950 to 1969. The lowest temperature recorded during that period was also −100 °F (−73 °C).[120]
Subpeaks and nearby mountains
[edit]
Besides the North Summit mentioned above, other features on the massif which are sometimes included as separate peaks are:
- South Buttress, 15,885 feet (4,842 m); mean prominence: 335 feet (102 m)
- East Buttress high point, 14,730 feet (4,490 m); mean prominence: 380 feet (120 m)
- East Buttress, most topographically prominent point, 14,650 feet (4,470 m); mean prominence: 600 feet (180 m)
- Browne Tower, 14,530 feet (4,430 m); mean prominence: 75 feet (23 m)
Nearby peaks include:
Taxonomic honors
[edit]
- denaliensis
- Ceratozetella denaliensis (formerly Cyrtozetes denaliensis Behan-Pelletier, 1985) is a species of moss mite in the family Mycobatidae
- Magnoavipes denaliensis Fiorillo et al., 2011 (literally "bird with large feet found in Denali") is a Magnoavipes ichnospecies of bird footprint from the Upper Cretaceous of Alaska and was a large heron-like bird (as large as a sandhill crane) with three toes and toe pads.
- denali
- Cosberella denali (Fjellberg, 1985) is a springtail in the genus Cosberella.
- Proclossiana aphirape denali Klots, 1940 is a Boloria butterfly subspecies in the family Nymphalidae.
- Symplecta denali (Alexander, 1955) is a species of crane fly in the family Limoniidae.
- Tipula denali Alexander, 1969 is a species of crane fly in the family Tipulidae.
- denalii
- Erigeron denalii A. Nelson, 1945 or Denali fleabane is an Erigeron fleabane species.
- mckinleyensis or mackinleyensis
- Erebia mackinleyensis (Gunder, 1932) or Mt. McKinley alpine is a butterfly species of the subfamily Satyrinae of family Nymphalidae.
- Oeneis mackinleyensis Dos Passos 1965 or Oeneis mckinleyensis Dos Passos 1949 is a butterfly species of the subfamily Satyrinae of family Nymphalidae (synonym of Oeneis bore)
- Uredo mckinleyensis Cummins 1952 (sometimes spelled Uredo mackinleyensis) is a rust fungus species.
- others:
- Papaver mcconnellii Hultén 1945, synonym Papaver denalii Gjaerevoll 1963, is a poppy species.
In popular culture
[edit]- In 2019, American educational animated series Molly of Denali premiered on PBS and CBC Kids. The show depicts the daily life and culture of Molly, a young Alaskan Native girl and vlogger.[121][122][123] The animated series has received acclaim for its representation of Indigenous Alaskan culture.[124][125]
See also
[edit]References
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The State of Alaska changed the name of the mountain to Denali in 1975, although the U.S. Board on Geographic Names has continued to use the name Mount McKinley. Today most Alaskans refer to Mount McKinley as Denali.
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- Secor, R. J. (1998). Denali Climbing Guide. Mechanicsburg, Pennsylvania: Stackpole Books. ISBN 0-8117-2717-3. Retrieved February 16, 2013.
- Stuck, Hudson (1914). The ascent of Denali (Mount McKinley): a narrative of the first complete ascent of the highest peak in North America. C. Scribner's Sons. OCLC 1507759. Retrieved September 14, 2025 – via Archive.org. ISBN 978-0-935632-69-9
- Washburn, Bradford; Roberts, David (1991). Mount McKinley: the conquest of Denali. Abrams Books. ISBN 978-0-8109-3611-9.
- Waterman, Jonathan; Washburn, Bradford (1988). High Alaska: A Historical Guide to Denali, Mount Foraker, & Mount Hunter. The Mountaineers Books. ISBN 978-0-930410-41-4. Retrieved February 16, 2013.
- Waterman, Jonathan (1998). In the Shadow of Denali: Life and Death on Alaska's Mt. McKinley. Lyons Press. ISBN 978-1-55821-726-3. Retrieved February 4, 2013.
- Waterman, Jonathan (1991). Surviving Denali: A Study of Accidents on Mt. McKinley, 1910-1990. The Mountaineers Books. ISBN 978-1-933056-66-1. Retrieved February 16, 2013.
- Wilson, Rodman; Mills, William J. Jr.; Rogers, Donald R.; Propst, Michael T. (June 1978). "Death on Denali". Western Journal of Medicine. 128 (6): 471–76. LCCN 75642547. OCLC 1799362. PMC 1238183. PMID 664648.
Further reading
[edit]- Drury, Bob (2001). The Rescue Season: A True Story of Heroism on the Edge of the World. New York: Simon & Schuster. ISBN 0-684-86479-7. OCLC 44969545. Also titled The Rescue Season: The Heroic Story of Parajumpers on the Edge of the World. About the US Air Force's 210th Rescue Squadron during the 1999 climbing season on Denali.
External links
[edit]- Mt. McKinley Weather Station
- Denali at SummitPost
- Timeline of Denali climbing history, National Park Service Archived July 5, 2007, at the Wayback Machine
- The Ascent of Denali (Mount McKinley) at Project Gutenberg
- Mount Mckinley Quadrangle Publications, Alaska Division of Geological & Geophysical Surveys
Denali
View on GrokipediaPhysical Characteristics
Geological Formation and Structure
Mount McKinley forms part of the central Alaska Range, a 600-mile (970 km) east-west trending arc of mountains resulting from the accretion and deformation of disparate crustal terranes during Mesozoic and Cenozoic tectonic events.[7] The range's uplift stems from ongoing oblique subduction of the Pacific Plate beneath the North American Plate, occurring at a convergence rate of approximately 7 cm per year, which compresses and elevates continental crust through thrust faulting and crustal shortening.[8] This process has wrinkled and folded ancient terranes—fragments of oceanic and continental crust from thousands of miles away—into the range's spiny backbone, with Mount McKinley representing the highest point due to localized structural resistance.[1] The mountain's core consists of a resistant granitic pluton, primarily quartz monzonite and granite from a larger batholith intruded deep within the crust during subduction-related magmatism, likely in the Late Cretaceous period.[1] This igneous rock, less dense than surrounding materials, "floats" upward under tectonic pressure and resists erosion, preserving Mount McKinley's steep topography as it rises about 3.5 miles (5.6 km) above its base elevation of roughly 2,000 feet (610 m).[1] Surrounding the pluton are metamorphic rocks such as schist, slate, quartzite, and marble, formed under high pressure and temperature from pre-existing sedimentary and volcanic protoliths, alongside minor sedimentary layers bearing fossils from ancient marine environments.[1] Structurally, Mount McKinley's elevation is enhanced by two key faults: the Mount McKinley Fault, a right-lateral strike-slip system extending over 2,000 miles, which offsets terrain westward at 1 cm per year and features a northward-convex bend near the mountain that induces transpressional compression, piling up crustal blocks; and the parallel Hines Creek Fault, a thrust fault that overrides northern blocks southward, amplifying vertical uplift.[8] These faults dissect the range into northern, central, and southern terranes, with Mount McKinley straddling the central segment where fault interactions concentrate deformation.[1] The current uplift rate measures about 0.5 mm per year, indicating continued growth amid active tectonics, potentially adding 1 km of height over the next 2 million years if rates persist.[1][8] Glacial erosion has further sculpted the structure, carving cirques, horns, and U-shaped valleys, though the underlying plutonic and metamorphic framework dictates its overall form.[7]Elevation, Topography, and Measurement
Mount McKinley reaches a summit elevation of 20,310 feet (6,190 meters) above sea level, establishing it as the highest mountain in North America.[9] This measurement surpasses all other peaks on the continent, including Mount Logan in Canada at 19,551 feet (5,959 meters).[9] The mountain's base lies approximately 2,000 feet (610 meters) above sea level near the confluence of the Kahiltna and Tokositna Glaciers, yielding a total vertical rise from base to summit of about 18,000 feet (5,500 meters), the greatest such rise for any mountain on land.[10] Topographically, Mount McKinley forms a massive, glaciated massif within the Alaska Range, characterized by steep, ice-covered slopes exceeding 40 degrees in places and extensive glacier systems covering over 25% of its surface.[10] Its topographic prominence measures 20,156 feet (6,144 meters), defined as the height difference between the summit and the lowest contour line encircling it without including higher peaks, positioning Mount McKinley as the third-most prominent peak worldwide after Mount Everest and Aconcagua.[11] This prominence arises from its isolation within a restraining bend of the Mount McKinley Fault, a major strike-slip fault system displacing at about 7 millimeters per year, which has uplifted the mountain 3,000 meters (9,800 feet) above surrounding terrain over millions of years.[10] The peak's broad summit plateau contrasts with its abrupt western and southern faces, while the eastern Kahiltna Glacier descends dramatically, contributing to its rugged, pyramidal profile visible from distances up to 150 miles (240 kilometers) on clear days. The official elevation derives from a 2015 U.S. Geological Survey (USGS) effort employing GPS receivers, satellite interferometry, and ground-based surveys, which adjusted the longstanding figure of 20,320 feet (6,194 meters)—established via 1950s photogrammetry—downward by 10 feet.[9] This recalculation involved a team of surveyors and climbers who ascended to high camps to collect precise data under challenging arctic conditions, cross-verifying with airborne lidar and gravity measurements to account for crustal motion and erosion.[9] Earlier assessments, such as Robert Muldrow's 1898 trigonometric survey yielding 20,300 feet (6,200 meters), relied on less accurate optical instruments and baseline assumptions prone to error from atmospheric refraction and instrument calibration.[12] These historical methods underscore the evolution toward satellite-based precision, which minimizes uncertainties to within a few feet while confirming Mount McKinley's dominance over North American rivals.[9]Surrounding Terrain and Subpeaks
Mount McKinley occupies the central segment of the Alaska Range, a 600-mile (970 km) arc-shaped chain of mountains stretching from the Alaska-Yukon border to the Alaska Peninsula, with its highest elevations concentrated in Denali National Park and Preserve. This region features a dramatic landscape of steep ridges, deep valleys, and extensive ice fields, shaped by tectonic uplift along the Mount McKinley Fault and ongoing glacial erosion. The terrain rises sharply from surrounding lowlands around 2,000 feet (610 m) elevation, with Mount McKinley itself ascending over 18,000 feet (5,500 m) above its base, creating extreme relief unparalleled in North America.[1] The mountain's flanks are drained by massive glaciers, including the Kahiltna Glacier—the longest in the Alaska Range at 44 miles (71 km)—which flows southwestward from near the summit, and the Muldrow Glacier extending northeast. These ice masses, some reaching thicknesses of 3,700 feet (1,130 m), radiate outward like spokes, covering over 75% of Mount McKinley's surface and one million acres (400,000 hectares) of the park, influencing local climate and hydrology through their reflective albedo and meltwater contributions. Adjacent peaks such as Mount Foraker and Mount Hunter form a cluster of ultra-prominent summits, contributing to the area's frequent high winds exceeding 100 mph (160 km/h) and katabatic flows.[13][14][1] Mount McKinley's structure includes a north-south trending summit ridge, with the principal South Peak at 20,310 feet (6,190 m) and the subsidiary North Peak at 19,470 feet (5,934 m), separated by a col at approximately 18,600 feet (5,670 m). Other notable subpeaks on the massif, such as Archdeacons Tower rising to about 19,600 feet (5,974 m), add to its complex topography, while sheer faces like the 14,000-foot (4,270 m) Wickersham Wall drop from the North Peak toward the Peters Glacier below. These features, forged from granitic and metamorphic rocks, underscore the mountain's role as a focal point of the range's orogenic history.[15][1]Nomenclature Disputes
Indigenous and Pre-Colonial Designations
The tallest peak in North America, located in south-central Alaska, held distinct designations among indigenous Athabascan peoples who inhabited the surrounding regions for millennia prior to European contact.[6] These groups, including the Koyukon, Dena'ina, Ahtna, Upper Kuskokwim, and Lower Tanana, each employed unique names reflecting the mountain's imposing stature, with no singular pan-indigenous term in widespread use.[6] At least nine Alaska Native groups are documented as having referenced the peak in their oral traditions and place-name systems, often in contexts of hunting and seasonal migration across its flanks and foothills.[6] Among the Koyukon Athabascans, whose territory extended northward along the Yukon River, the mountain was called Denali, derived from deenaalee or deenaali, translating to "the high one" or "the tall one," emphasizing its elevation relative to surrounding terrain.[16] In contrast, the Dena'ina Athabascans of the Susitna River valley to the south referred to it as Dghelay Ka'a (sometimes anglicized as Doleika or Traleika), meaning "big mountain" or "the object hangs low," a descriptor possibly alluding to its massive profile dominating the horizon.[17] [18] Further variations existed among proximate groups: the Upper Kuskokwim Athabascans termed it Denaze, while Ahtna speakers and Lower Tanana peoples used linguistically related but distinct appellations tied to their dialects, all rooted in five principal Athabascan languages spoken near the mountain's base.[19] [6] These pre-colonial names, preserved through oral histories rather than written records, underscore the mountain's role as a navigational and spiritual landmark in indigenous subsistence economies, though direct evidence of ascents or ritual use remains anecdotal and unverified by archaeological finds.[20] The popularized use of "Denali" in modern discourse stems primarily from the Koyukon term, despite the peak's location overlapping Dena'ina and other territories, highlighting how linguistic borrowing has sometimes overshadowed regional specificity in non-native retellings.[21]Adoption of Mount McKinley Name
In August 1896, amid the early stirrings of the Klondike Gold Rush, prospector William A. Dickey led an expedition along the Susitna River in Alaska Territory and applied the name Mount McKinley to the region's dominant peak, honoring William McKinley, the recently nominated Republican presidential candidate from Ohio who advocated for the gold standard—a monetary policy aligning with the interests of gold seekers like Dickey.[22] Dickey, originally from New Hampshire and then based in Seattle, documented the naming in a published account, declaring: "We named our great peak Mount McKinley, after William McKinley of Ohio, who had been nominated for the Presidency, and that fact was the first news we had received in that far northern land."[23] This designation disregarded longstanding indigenous Athabascan nomenclature, such as "Denali" meaning "the high one," but reflected the era's pattern of Euro-American explorers imposing politically expedient labels on geographic features.[16] The name's adoption accelerated through Dickey's publicity in outlets like the New York Sun in early 1897, which disseminated it to broader audiences during McKinley's successful campaign and presidency (1897–1901).[24] McKinley himself held no personal ties to Alaska—he never visited the territory—and the honor stemmed primarily from Dickey's partisan enthusiasm rather than any substantive connection, though McKinley's pro-gold stance resonated with prospectors facing economic uncertainties from silver advocacy by opponents like William Jennings Bryan.[22] By the early 1900s, maps, surveys, and expedition reports increasingly used "Mount McKinley," supplanting earlier vague references like "Densmore's Mountain" from 1890 U.S. Army surveys, as non-native settlement and federal interest in Alaska grew.[25] Federal formalization occurred on February 26, 1917, when President Woodrow Wilson signed the Mount McKinley National Park Act, establishing a national park around the peak and enshrining "Mount McKinley" in official U.S. nomenclature for the first time, amid broader efforts to conserve Alaskan wilderness and promote tourism. This act, driven by conservationists like Stephen Mather of the nascent National Park Service, locked in the name for federal use, including USGS mappings, despite ongoing local preferences for indigenous terms and without consultation of Alaska Native groups. The designation endured as the mountain's primary identifier in government documents, scientific literature, and popular media for nearly a century, reflecting the dominance of English-language, politically influenced naming conventions in American territorial expansion.[16]2015 Federal Renaming to Denali
In 1975, the Alaska State Legislature passed a resolution renaming the mountain Denali, reflecting its longstanding designation among Alaska Native peoples, though the federal government continued to recognize Mount McKinley officially.[6] On August 30, 2015, U.S. Secretary of the Interior Sally Jewell announced that the Department of the Interior had approved the change of the federal name from Mount McKinley to Denali, following a review by the U.S. Board on Geographic Names.[26] [22] The decision aligned federal nomenclature with Alaska's 40-year-old designation and recognized "Denali," a Koyukon Athabascan term meaning "the high one" or "the tall one," used by indigenous Alaskans for centuries to describe the peak.[26] [6] The announcement occurred during President Barack Obama's visit to Alaska, where he highlighted climate change impacts in the region, though the renaming was presented as a separate act of cultural reverence independent of broader policy agendas.[27] [28] Jewell stated that the change honored "the traditions of Alaska’s original people" and local usage, noting that the peak had been mapped as Denali by early explorers like James Wickersham in 1903 before the McKinley name gained federal traction.[26] [6] The U.S. Board on Geographic Names, responsible for standardizing domestic names, had previously resisted the change due to the historical precedent of the 1917 federal adoption of Mount McKinley, named after President William McKinley by prospector William A. Dickey in 1896 as a political gesture amid the Klondike Gold Rush, despite McKinley's lack of direct connection to Alaska.[29] [22] The renaming drew immediate bipartisan criticism, particularly from Ohio Republicans, McKinley's home state, who argued it disrespected the 25th president and undermined congressional intent in the 1917 naming.[30] Ohio Governor John Kasich called it "wrong," while Representative Bill Johnson introduced legislation to block it, asserting that McKinley deserved recognition for his economic policies and that the change bypassed legislative oversight.[31] Supporters, including Alaskan officials and Native leaders, welcomed the move as correcting a politically motivated imposition, emphasizing that indigenous names predated European contact and that federal consistency with state practice resolved long-standing confusion in mapping and signage.[27] [22] No formal congressional reversal occurred at the time, and the name Denali persisted federally until subsequent administrative changes.[29]2025 Reversion to Mount McKinley
On January 20, 2025, President Donald Trump signed Executive Order 14000, titled "Restoring Names That Honor American Greatness," directing the Secretary of the Interior to revert the federal name of North America's highest peak from Denali to Mount McKinley, honoring the 25th U.S. President William McKinley.[2] The order specified that the surrounding Denali National Park and Preserve would retain its name, distinguishing the mountain's designation from the protected area's title.[2] This action reversed the 2015 renaming under President Barack Obama, which had been implemented by executive authority without congressional approval, prompting critics to argue it exemplified unilateral federal overreach on geographic nomenclature.[32] The rationale, as stated in the executive order and Trump's public remarks, emphasized restoring a name tied to American historical figures over indigenous terms, framing it as a correction to prior administrations' decisions that prioritized cultural revisions at the expense of national heritage.[33] Trump had pledged this reversion during his 2024 campaign, citing McKinley's legacy in economic policy and expansionism, and positioned the change alongside other renamings like the Gulf of Mexico to "Gulf of America" to symbolize patriotic reclamation.[34] Supporters, including some conservative commentators, viewed it as rejecting what they described as politically motivated erasures of Euro-American history, though the order's implementation relied on the same Interior Department processes used in 2015, raising questions about the consistency of executive precedent in naming disputes.[35] Reactions were sharply divided, with strong opposition from Alaskan officials and indigenous groups who argued the change disregarded local usage and Athabascan heritage, where "Denali" (meaning "the high one") had been employed for millennia.[36] On February 7, 2025, the Alaska Legislature passed a resolution urging Trump to retain "Denali," reflecting bipartisan state preference established since Alaska's 1975 legislative recognition of the name.[37] U.S. Senators Lisa Murkowski and Dan Sullivan, both Republicans, introduced S. 512 on February 13, 2025, to codify "Denali" federally and override the executive action, highlighting tensions between state sovereignty and federal directive. Mountaineering communities, including the American Alpine Club, largely dismissed the change, asserting that climbers and guides would continue using "Denali" based on practical tradition rather than bureaucratic fiat.[38] As of October 2025, the federal designation remains Mount McKinley on U.S. Geological Survey maps and official documents, with the Geographic Names Information System (GNIS) listing Mount McKinley as the primary name and Denali as an alternate, though no major legal challenges had overturned it, and informal usage in Alaska and among indigenous populations persisted with "Denali."[39][40] The reversion underscored ongoing debates over nomenclature authority, with proponents of the change citing executive consistency and opponents decrying it as symbolic overreach amid broader cultural policy shifts.[41]Historical Exploration
Early Sightings and Surveys
The first recorded European sighting of Mount McKinley occurred on May 6, 1794, when British explorer George Vancouver observed the mountain's distant peaks from the Cook Inlet during his survey of the Alaskan coast; he described them in his journal as "stupendous snow mountains" visible on the northern horizon.[25] [42] Vancouver's expedition did not approach the interior, limiting the observation to a remote visual identification amid the Alaska Range.[25] Subsequent 19th-century sightings were sporadic, primarily by prospectors amid the Alaska Gold Rush. In 1889, Frank Densmore, a miner exploring the Toklat River drainage, reported the first close-range Western view of the peak from approximately 50 miles away, noting its immense scale and snow-covered dome dominating the skyline.[25] These accounts, while anecdotal, marked initial non-indigenous recognition of the mountain's prominence, though accurate mapping remained elusive due to the remote terrain and lack of triangulation data.[20] Early surveys began in the late 1890s under the U.S. Geological Survey (USGS), driven by mineral resource assessments following Alaska's territorial acquisition. In 1898, USGS geologist George Eldridge led an eight-man party that traversed the Susitna River valley, approaching within view of Mount McKinley's flanks and collecting preliminary topographic notes, though weather obscured precise measurements.[43] More systematic effort came in 1902, when USGS chief Alaskan geologist Alfred H. Brooks conducted a reconnaissance expedition, becoming the first documented non-indigenous person to set foot on the mountain's lower slopes at around 7,500 feet elevation on August 6; his team mapped glacial features and estimated the peak's height at over 20,000 feet based on barometric readings and angular observations.[44] [45] Brooks' work established foundational geospatial data, highlighting the peak's isolation and extreme relief relative to surrounding valleys.[46] These surveys prioritized scientific documentation over ascent, revealing Mount McKinley's geological context within the Alaska Range but underscoring measurement challenges from ground-based methods alone.[44]19th-Century Expeditions
In the mid-19th century, Russian explorer Lavrenty Zagoskin conducted surveys along the Tanana and Kuskokwim rivers during 1842–1844, likely becoming the first European to sight Mount McKinley from a distance while mapping interior Alaska. American traders Arthur Harper and Alfred Mayo provided the first confirmed non-native close-range sighting in 1878 while ascending the Tanana River in search of fur-trading opportunities, describing the peak's massive scale from the northern foothills.[47] The late 19th century saw increased activity driven by the Alaska gold rush, with prospectors penetrating the Alaska Range's periphery after 1880, drawn by rumors of mineral wealth; these informal parties reached the mountain's base but focused on resource assessment rather than ascent.[48] U.S. Geological Survey teams, beginning reconnaissance in the region around 1898, documented the terrain and geology surrounding the peak, contributing early topographic data amid the Klondike influx that brought hundreds of miners to nearby Kantishna and Toklat areas by 1898.[49] In 1896, prospector William A. Dickey, exploring for coal and gold near the Susitna River, named the mountain Mount McKinley after the Republican presidential candidate William McKinley, a designation that gained traction despite lacking official authority at the time.[22] The U.S. Army's 1899 expedition under 1st Lt. Joseph S. Herron marked the first non-native overland traverse of the Alaska Range via the Yentna and Kichatna rivers, producing maps and reports on the challenging glacial approaches to Mount McKinley's flanks, though the party did not attempt the summit and retreated due to harsh conditions.[25] These efforts yielded no summit attempts or high-altitude forays, limited instead by rudimentary equipment, extreme weather, and logistical barriers; they prioritized mapping and prospecting over mountaineering, setting the stage for 20th-century climbs while confirming the peak's isolation and elevation estimates exceeding 18,000 feet through distant triangulation.[48][49]20th-Century First Ascents
The first recorded ascent of Mount McKinley's North Peak occurred on April 3, 1910, during the Sourdough Expedition, led by prospectors including Pete Anderson, Billy Taylor, Charlie McGonagall, and Tom Lloyd.[25] Approaching via the Muldrow Glacier, the group summited the 19,740-foot (6,020 m) North Peak after a demanding climb without supplemental oxygen or modern gear, planting a 14-foot spruce pole topped with a reindeer antler as a marker. Initially met with skepticism and labeled a hoax due to lack of photographic evidence, the claim gained credibility in 2022 with the discovery of mislabeled photographs from the expedition at the University of Alaska Fairbanks, supporting the route and summit details.[50] This effort preceded any verified climb of the higher South Peak and highlighted the capabilities of local Alaskans in extreme conditions. The first undisputed ascent of Mount McKinley's South Peak, the mountain's true summit at 20,310 feet (6,190 m), took place on June 7, 1913, led by Episcopal Archdeacon Hudson Stuck and mountaineer Harry Karstens, with Native guide Walter Harper and physician Robert Tatum.[4] Starting from Nenana, the team traversed the Kantishna Glacier and ascended the South Buttress route, reaching the summit after 18 days of travel; Harper, of Athabascan descent, was the first to stand atop due to his position at the front.[51] Stuck documented the climb in his 1914 book The Ascent of Denali, emphasizing logistical challenges like crevasses, avalanches, and high winds, without fixed ropes or ice axes beyond basic tools.[52] This achievement resolved prior unverified claims, such as Frederick Cook's disputed 1906 report, establishing a benchmark for North American mountaineering.[53] Subsequent 20th-century firsts included the inaugural winter ascent of the South Peak on February 28, 1961, by Art Davidson, Ray Genet, and Dave Johnston via the West Buttress route.[54] Enduring temperatures below -40°F (-40°C) and gale-force winds that pinned them in a storm at 18,200 feet for five days, the trio summited without oxygen support, marking a milestone in high-latitude extreme climbing.[54] These expeditions underscored Mount McKinley's role as a proving ground for endurance and adaptation, influencing safety standards for future attempts.Climbing and Mountaineering
Major Routes and Techniques
The West Buttress route represents the primary and most accessible path for ascending Mount McKinley, originating from the Kahiltna Glacier base camp at approximately 7,200 feet (2,200 meters) and spanning about 14 miles (23 kilometers) round trip with over 13,000 feet (4,000 meters) of elevation gain.[55] This route features a series of established camps at elevations of 7,800 feet, 10,400 feet, 14,000 feet, 17,300 feet, and high camp near 17,800 feet, emphasizing gradual acclimatization through repeated ascents and descents for caching supplies.[56] Key sections include the Heartbreak Hill ascent, crevasse fields on the lower glacier, and steeper ice slopes up to 40 degrees near the summit ridge, where fixed ropes are commonly installed by ranger teams for safety.[57] Climbing techniques on the West Buttress prioritize glacier travel and hazard mitigation over rock climbing, involving roped teams for crevasse navigation, self-arrest with ice axes, and prusiking on fixed lines during high winds or whiteouts that can reduce visibility to zero.[58] Participants haul sleds laden with 100-150 pounds of gear and provisions, necessitating strong endurance training for pulling loads on snowshoes or skis, while managing extreme cold—often below -40°F (-40°C) with wind chills to -100°F (-73°C)—requires specialized insulated clothing, vapor barrier systems, and hot water for hydration to prevent frostbite and hypothermia.[59] Crevasse rescue drills, including Jumar ascenders and hauling systems, form essential prerequisites, as falls into hidden fissures remain a leading injury cause despite probing and bridging tactics.[60] Alternative routes include the Muldrow Glacier from the north, a longer 30-mile approach via McGonagall Pass that follows the historic first-ascent path but demands greater self-sufficiency due to remoteness and variable serac hazards.[61] The West Rib offers a steeper, more direct line with mixed ice and rock sections requiring advanced crampon work and short pitches of technical climbing.[58] For experienced alpinists, the Cassin Ridge on the south face presents the most demanding option, featuring 8,000 feet of continuous steep snow, ice, and rock terrain graded at 5.8 to 5.10 in difficulty, first ascended in 1961 and involving multi-pitch leads, belays, and exposure to rockfall and avalanches.[61] These routes collectively underscore Mount McKinley's expedition-style demands, where success rates hover around 50% for West Buttress attempts, influenced by weather windows typically lasting 1-3 days amid frequent storms.[57]Notable Expeditions and Records
The first successful ascent of Mount McKinley occurred on June 7, 1913, led by Episcopal Archdeacon Hudson Stuck, with Harry Karstens, Walter Harper (a Native Alaskan of Athabascan descent who reached the summit first), and Robert Tatum. The team approached via the South Buttress route, establishing camps up to 18,000 feet, and confirmed the mountain's height at 20,300 feet using an aneroid barometer. This expedition resolved earlier disputed claims, such as Frederick Cook's 1906 assertion, which lacked verifiable evidence and was later debunked by surveys.[62][52] The first winter ascent was achieved on February 28, 1967, by Art Davidson, Ray Genet, and Dave Johnston via the South Buttress. Facing temperatures below -40°F and high winds, they endured a perilous descent, including a bivouac at 18,200 feet without shelter during a storm. This milestone highlighted Mount McKinley's extreme winter conditions, where success rates remain low due to hypothermia risks and avalanche dangers.[25][54] Charlie Porter completed the first solo ascent in May 1976, climbing the Cassin Ridge in approximately 36 hours from advanced base camp. Porter's alpine-style effort, relying on minimal gear and fixed lines from prior parties, demonstrated advanced technical proficiency on steep ice and rock pitches up to 5.9 difficulty.[51] Vern Tejas accomplished the first solo winter ascent and survival on March 6, 2018, wait no, 1988, via the West Buttress, starting February 16 and enduring solo camps in temperatures to -59°F. Previous attempts, like Naomi Uemura's 1984 solo winter summit, ended in fatality on descent, underscoring the endeavor's risks. Tejas's success involved self-rescue techniques and radio coordination with rangers.[63][64] Modern speed records focus on fastest known times (FKTs) from 7,200-foot base camp on the West Buttress. Jack Kuenzle set the current round-trip FKT of 10 hours 14 minutes 57 seconds on June 5, 2023, using skis for descent. This surpassed Karl Egloff's 11:44 ski-less effort in 2019 and Kilian Jornet's 11:48 in 2014, emphasizing endurance in variable weather and crevasse fields.[65][66] Other notable records include the 1979 first ascent by dog team, led by Susan Butcher with Joe Redington Sr., Ray Genet, Brian Okonek, and Robert Stapleton, covering the West Buttress in sub-zero conditions. Mount McKinley's climbing history also features high fatality rates, with over 120 deaths since 1903, often from falls (45%) and exposure, though these inform safety records rather than ascents.[67]Safety Protocols and Hazards
Climbing Mount McKinley presents severe hazards due to its extreme environmental conditions, including temperatures dropping to -40°F (-40°C) or lower, winds exceeding 100 mph (160 km/h), and frequent whiteout storms that can persist for days.[68] Objective dangers such as avalanches, crevasses, and icefalls are prevalent, particularly on routes like the West Buttress, where unstable snow bridges over hidden crevasses pose risks of sudden collapse.[69] Falls from steep terrain or during fixed-line sections have caused at least 14 deaths on the West Buttress since 1980, often due to fatigue, poor visibility, or equipment failure.[70] Altitude-related illnesses, including high-altitude pulmonary edema (HAPE) and cerebral edema (HACE), compound these threats, as rapid ascents above 14,000 feet (4,267 m) exacerbate hypoxia without proper acclimatization.[71] Hypothermia and frostbite remain leading non-traumatic causes of injury, with climbers exposed to prolonged wind chill factors below -100°F (-73°C); dehydration from dry Arctic air further impairs judgment and physical performance.[72] Since 1932, at least 129 fatalities have occurred on Mount McKinley, with a historical fatality rate of approximately 3.08 per 1,000 summit attempts, though this has declined due to improved gear and awareness.[73] In 2024 alone, multiple incidents included falls and presumed avalanches, highlighting ongoing risks even for experienced teams.[74] Solo climbers face amplified dangers, as undetected crevasse falls or avalanches lack immediate rescue potential, with park rangers noting that bridge strength over voids cannot be reliably assessed without partners.[75] Safety protocols enforced by Denali National Park mandate advance registration and permits for all climbers attempting Mount McKinley or Mount Foraker, requiring submission at least 60 days prior via the NPS Pay.gov system to allow review of plans and climber qualifications.[76] Permit fees for 2025 are $340 for individuals aged 24 and under, with higher rates for older climbers, and include requirements for detailed itineraries, emergency plans, and proof of experience such as prior high-altitude climbs.[77] Climbers must attend an orientation in Talkeetna, Alaska, where rangers brief on current conditions, mandatory gear (e.g., stoves for melting snow, crevasse rescue kits, and satellite communication devices), and prohibitions like solo ascents above certain elevations without approval.[78] Acclimatization schedules, typically involving multiple camps at 7,800 feet (2,377 m), 11,000 feet (3,353 m), and 14,200 feet (4,333 m), are recommended to mitigate altitude sickness, alongside strict waste management rules to prevent environmental contamination.[79] Guided expeditions, offered by NPS-permitted outfitters, incorporate additional safeguards like professional guides trained in crevasse rescue, weather monitoring via aviation support, and medical evacuation protocols, significantly reducing fatality risks compared to independent teams.[80] Park rangers conduct patrols and monitor via radio, but self-reliance is emphasized, as rescue operations—often involving helicopters or fixed-wing aircraft—are weather-dependent and occur only after climbers activate personal locator beacons.[81] Violations of protocols, such as inadequate gear or unpermitted climbs, result in permit revocation and potential fines, underscoring the NPS's focus on preparation to counter Mount McKinley's unforgiving conditions.[59]Recent Climbing Seasons and Incidents
In recent years, Mount McKinley's climbing season, typically spanning mid-May to mid-July, has featured fluctuating summit success rates amid persistent challenges from high winds, rapid weather shifts, and avalanche risks. For the 2025 season, 962 climbers registered, with roughly 35%—approximately 337—reaching the summit, a rate depressed by a severe storm on June 25–26 that deposited significant snow across elevations, prompting an early closure by mid-July and stranding teams below key camps.[82][83][84] The prior year, 2024, saw 974 registrants and 511 summits for a 52% success rate, with 639 U.S. and 362 international participants averaging 14 days for independent teams and 17 days for guided ones.[85][86] In 2023, amid poor weather yielding a 30% summit rate, 670 U.S. and 351 international climbers attempted the peak, with women comprising 19% of teams and achieving a 63% success rate among them.[87][88][89] Fatalities and rescues underscore Mount McKinley's hazards, primarily unroped falls and avalanches on routes like the West Buttress. In 2025, two climbers died: Alex Chiu, 41, of Seattle, fell unroped over 3,000 feet from the West Buttress on June 4, with his body recovered by rangers; and Nicholas Vizzini, 29, from Washington state, triggered and perished in an avalanche while descending a slope on June 11.[90][91][92][93] An additional incident at Grizzly Gap on May 13 involved multiple climbers caught in an avalanche, resulting in injuries treated by rangers.[94] Multiple fatal falls occurred in 2024, per ranger assessments of 34 patients, though exact counts remain detailed in seasonal logs.[86] Earlier, 2023 recorded one avalanche death and one fatal fall, while 2022 saw three fatalities, including a solo climber who fell below Mount McKinley Pass.[88][95] These events highlight the mountain's objective dangers, with over 130 total historical deaths, about 13 from avalanches.[90]| Year | Registered Climbers | Approximate Summits | Summit Success Rate (%) | Reported Fatalities |
|---|---|---|---|---|
| 2025 | 962 | 337 | 35 | 2 (falls, avalanche) |
| 2024 | 974 | 511 | 52 | Multiple falls |
| 2023 | ~1,021 | ~306 | 30 | 2 (avalanche, fall) |
| 2022 | Not specified | Not specified | Not specified | 3 |
