| Denali National Park and Preserve | |
|---|---|
IUCN category V (protected landscape/seascape) | |
.jpg) Denali is the tallest peak in North America. | |
  Location in Alaska Show map of Alaska Location in North America Show map of North America | |
| Location | Denali Borough andMatanuska-Susitna Borough, Alaska, United States |
| Nearest city | Healy |
| Coordinates | 63°26′N150°19′W / 63.43°N 150.32°W /63.43; -150.32 |
| Area | 4,740,911 acres (19,185.79 km2) (park) and 1,304,242 acres (5,278.08 km2) (preserve)[1] |
| Established | February 26, 1917 |
| Visitors | 427,562 (in 2022)[2] |
| Governing body | National Park Service |
| Website | nps |
Denali National Park and Preserve, formerly known asMount McKinley National Park, is aUnited States national park andpreserve located inInterior Alaska, centered onDenali (federally designated as Mount McKinley), the highest mountain in North America. The park and contiguous preserve encompass 6,045,153 acres (2,446,387 ha; 9,446 sq mi; 24,464 km2) which is larger than the state ofNew Hampshire.[3] On December 2, 1980, 2,146,580-acre (3,354 sq mi; 8,687 km2) Denali Wilderness was established within the park. Denali's landscape is a mix of forest at the lowest elevations, including deciduoustaiga, withtundra at middle elevations, andglaciers, snow, and bare rock at the highest elevations. The longest glacier isKahiltna Glacier. Wintertime activities includedog sledding,cross-country skiing, andsnowmobiling. The park received 594,660 recreational visitors in 2018.
Human habitation in the Denali Region extends to more than 11,000 years before the present, with documented sites just outside park boundaries dated to more than 8,000 years before the present. However, relatively few archaeological sites have been documented within the park boundaries, owing to the region's high elevation, with harsh winter conditions and scarce resources compared to lower elevations in the area. The oldest site within park boundaries is the Teklanika River site, dated to about 7130 BC. More than 84 archaeological sites have been documented within the park. The sites are typically characterized as hunting camps rather than settlements and provide little cultural context. The presence ofAthabaskan peoples in the region is dated to 1,500 - 1,000 years before present on linguistic and archaeological evidence, while researchers have proposed that Athabaskans may have inhabited the area for thousands of years before then. The principal groups in the park area in the last 500 years include theKoyukon,Tanana andDena'ina people.[4]
In 1906, conservationistCharles Alexander Sheldon conceived the idea of preserving the Denali region as a national park. He presented the plan to his co-members of theBoone and Crockett Club. They decided that the political climate at the time was unfavorable for congressional action and that the best hope of success rested on the approval and support of the Alaskans themselves. Sheldon wrote, "The first step was to secure the approval and cooperation of the delegate who represented Alaska in Congress."[citation needed]
In October 1915, Sheldon took up the matter with E. W. Nelson of the Biological Survey at Washington, D.C., and withGeorge Bird Grinnell, with the purpose to introduce a suitable bill in the coming session of Congress. The matter was then taken to the Game Committee of the Boone and Crockett Club and, after a full discussion, it received the committee's full endorsement.
On December 3, 1915, the plan was presented to Alaska's delegate,James Wickersham, who after some deliberation gave his approval. The plan then went to the executive committee of the Boone and Crockett Club and, on December 15, 1915, it was unanimously accepted. The plan was thereupon endorsed by the club and presented toStephen Mather, Assistant Secretary of the Interior in Washington, D.C., who immediately approved it.
The bill was introduced in April 1916, by Delegate Wickersham in the House and by SenatorKey Pittman of Nevada in the Senate. Much lobbying took place the following year, and on February 19, 1917, the bill passed. On February 26, 1917, 11 years from its conception, the bill was signed in legislation by the President of the United States,Woodrow Wilson, thereby creating Mount McKinley National Park.[5][6]
A portion of Denali, excluding the summit, was included in the original park boundary. The boundary was expanded in 1922 and again in 1932[7] and 1947 to include the area of the hotel and railroad.
On Thanksgiving Day in 1921, the Mount McKinley Park Hotel opened.[8] In July 1923, PresidentWarren Harding stopped at the hotel, on a tour of the length of theAlaska Railroad, during which he drove a golden spike signaling its completion atNenana.[citation needed] The hotel was the first thing visitors saw stepping down from the train. The flat-roofed, two-story log building featured exposed balconies, glass windows, and electric lights. Inside were two dozen guest rooms, a shop, a lunch counter, a kitchen, and a storeroom. By the 1930s, there were reports of lice, dirty linen, drafty rooms, and marginal food, which led to the hotel eventually closing.[citation needed] After being abandoned for many years, the hotel was destroyed in 1972 by a fire.[7]
Fourteen log cabins were built in the late 1920s and early 1930s as a network of shelters for patrolling park rangers throughout the park. They were listed in theNational Register of Historic Places in 1986.[9]
The 93 mi (150 km) Park Road was completed in 1938 after 17 years of construction.[7]
There was no road access to the park entrance until 1957 when theDenali Highway opened; park attendance greatly expanded: there were 5,000 visitors in 1956 and 25,000 visitors by 1958.[7] In 1971, theGeorge Parks Highway, under piecemeal construction for several years, was completed, providing direct highway connections to Anchorage and Fairbanks. Visitation doubled to 88,000 from 1971 to 1972.[7] With the increase in visitors, the park closed most of the Park Road that year to private vehicles and required visitors to take shuttle buses.[10]
In 1967, the park was the site of one of the deadliest mountaineering accidents in the United States with theMount McKinley disaster, where seven climbers died in an intenseblizzard on Denali. The Park Service debated closing the mountain to climbing in the wake of the accident, but ultimately it remained open.[11]
The park was designated aninternational biosphere reserve in 1976.[7] A surrounding Denali National Monumentwas proclaimed by PresidentJimmy Carter on December 1, 1978, which was combined with the park in 1980.
The name of Mount McKinley National Park was subject to local criticism from the beginning of the park. The word Denali means "the high one" in the nativeAthabaskan language and refers to the mountain itself. The mountain was named after newly elected US presidentWilliam McKinley in 1897 by local prospector William A. Dickey. The United States government formally adopted the name Mount McKinley after President Wilson signed the bill creating Mount McKinley National Park in 1917.[12] In 1980, Mount McKinley National Park was combined with Denali National Monument, and theAlaska National Interest Lands Conservation Act named the combined unit the Denali National Park and Preserve. At that time the Alaska state Board of Geographic Names changed the name of the mountain to Denali. However, theU.S. Board on Geographic Names did not recognize the change and continued to denote the official name as Mount McKinley. This situation lasted until August 30, 2015, when PresidentBarack Obama directedSecretary of the InteriorSally Jewell to rename the mountain to Denali, using statutory authority to act on requests when the Board of Geographic Names does not do so in a "reasonable" period.[13] At the beginning of his second term, PresidentDonald Trump signed an executive order to revert the name of the mountain to Mount McKinley, while explicitly leaving the name of the national park and preserve unchanged.[14] Renaming the park requires an act of Congress.[citation needed]
In 1992,Christopher McCandless ventured into theAlaskan wilderness and settled in an abandonedbus in the park on theStampede Trail at63°52′5.96″N149°46′8.39″W / 63.8683222°N 149.7689972°W /63.8683222; -149.7689972 , near Lake Wentitika. He carried little food or equipment, and hoped tolive simply for a time in solitude. Almost four months later, McCandless'sstarved remains were found, weighing only 67 lb (30 kg). His story has been widely publicized viaarticles, books, and films, and the bus where his remains were found has become a shrine attracting people from around the world.[15]
On November 5, 2012, theUnited States Mint released the 15th of itsAmerica the Beautiful Quarters series, which honors Denali National Park. The coin's reverse side features a Dall sheep with Denali in the background.[16]
In September 2013, President Barack Obama signed theDenali National Park Improvement Act into law.[17] The statute allows theUnited States Department of the Interior to "issue permits formicrohydroelectric projects in the Kantishna Hills area of the Denali National Park and Preserve in Alaska"; it authorizes the Department of the Interior and a company called Doyon Tourism, Inc. to exchange some land in the area; it authorizes theNational Park Service (NPS) to "issue permits to construct a natural gas pipeline in the Denali National Park"; and it renames the existing Talkeetna Ranger Station theWalter Harper Talkeetna Ranger Station.[18] The National Parks Conservation Association supported the bill because the legislation "takes a thoughtful approach to protecting roadless Alaska, promoting renewable energy development, and honoring native Alaskans."[19]
On September 24, 2020, the Museum of The North[20] at theUniversity of Alaska (Fairbanks) announced it became the permanent home of McCandless's 'Magic Bus 142' where it will be restored and an outdoor exhibit will be created.[21]
Denali National Park and Preserve includes the central, highest portion of theAlaska Range, together with many of the glaciers and glacial valleys running southwards out of the range. To the north the park and preserve encompass the valleys of theMcKinley,Toklat, andForaker Rivers, as well as the Kantishna and Wyoming Hills. TheGeorge Parks Highway runs along the eastern edge of the park, crossing the Alaska Range at the divide between the valleys of theChultina River and theNenana River. The entrance to the park is about 11 mi (18 km) south ofHealy. The Denali Visitor Center and the park headquarters are located just inside the entrance. Preserve lands are located on the west side of the park, with one parcel encompassing areas of lakes in the Highpower Creek and Muddy River areas, and the second preserve area covering the southwest end of the high Alaska Range aroundMount Dall. In contrast to the park, where hunting is prohibited or restricted to subsistence hunting by local residents, sport hunting is allowed in the preserve lands.[22] Nikolai, Telida, Lake Minchumina, and Cantwell residents are authorized to hunt inside the park because large portions of these communities historically hunted in the area for subsistence purposes.[23]
The size and relative isolation of Denali lead to it generating its own weather.[24] As a consequence, it is often surrounded by clouds.[25] Locals sometimes use the phrase "the mountain is out" when it makes an appearance.[26] It is commonly said that only 30 percent of visitors to the park ever actually see Denali.[26][27][25][28][29] An additional estimate is that only 10 percent of visitors get to see the mountain unobscured from top to bottom.[25] Because the weather patterns are different, Denali is more frequently visible during winter months.[30] The Eielson Visitor Center has an etched outline of the peaks of Denali on the window facing the Denali that shows where the mountain would be if it were visible.[31]
The Denali Wilderness is a wilderness area within Denali National Park that protects the higher elevations of the centralAlaska Range, includingDenali, federally designated as Mount McKinley. The wilderness comprises about one-third of the current national park and preserve—2,146,580 acres (3,354 sq mi; 8,687 km2) that correspond with the former park boundaries before 1980.[32]
Denali National Park and Preserve is located in the central area of the Alaska Range, a mountain chain extending 600 miles (970 km) across Alaska. Its best-known geologic feature is Denali, federally designated as Mount McKinley. Its elevation of 20,310 ft (6,190.5 m) makes it the highest mountain in North America. Its vertical relief (distance from base to peak) of 18,000 ft (5,500 m) is the highest of any mountain in the world. The mountain is still gaining about 1 mm (0.039 in) in height each year due to the continued convergence of theNorth American andPacific Plates. The mountain is primarily made ofgranite, a hard rock that does not erode easily; this is why it has retained such a great height rather than being eroded.
The park area is characterized bycollision tectonics: over the past millions of years, exoticterranes in the Pacific Ocean have been moving toward the North American landmass and accreting, or attaching, to the area that now makes up Alaska. The oldest rocks in the park are part of theYukon-Tanana terrane. They originated from ocean sediments deposited between 400 million and 1 billion years ago. The original rocks have been affected by the processes of regional metamorphism, folding, and faulting to form rocks such asschist,quartzite,phyllite,slate,marble, andlimestone. The next oldest group of rocks is the Farewell terrane. It is composed of rocks from thePaleozoic era (250–500 million years old). The sediments that make up these rocks were deposited in a variety of marine environments, ranging from deep ocean basins to continental shelf areas. The abundant marine fossils are evidence that around 380 million years ago, this area had a warm, tropical climate. The Pingston, McKinley, and Chulitna terranes are the next oldest; they were deposited in theMesozoic era. The rock types include marble,chert, limestone,shale, andsandstone. There are intrusions ofigneous rocks, such asgabbro,diabase, anddiorite. Special features includepillow basalts, which are formed when molten lava flows into water and a hard outer crust forms, making a puffy, pillow-shaped feature; as well as anophiolite sequence, which is a distinct sequence of rocks indicating that a section of the oceanic crust has been uplifted and thrust onto a continental area.
Some of the youngest rocks in the park include the Kahiltna terrane, which is aflysch sequence (a sedimentary rock sequence deposited in a marine environment during the early stages of mountain building) formed about 100 million years ago, during lateCretaceous time. Another rock sequence is the McKinley Intrusive Sequence, which includes Denali. TheCantwell Volcanics includebasalt andrhyolite flows, as well as ash deposits. An example can be seen atPolychrome Pass in the park.[33]
Mesozoic fossils includefossil trackways fromtherizinosaurids andhadrosaurids in theCantwell Formation indicate the area was once an immigration point fordinosaurs traveling between Asia and North America during theLate Cretaceous period. Studies of fossil plants from the same formation indicate the area was wet, with marshes and ponds throughout the region.[34]
Denali National Park and Preserve are located in an area of intense tectonic activity: thePacific Plate is subducting under theNorth American Plate, creating theDenali Fault system, which is a right-lateralstrike-slip fault over 720 miles (1,160 km) long. This is a part of the larger fault system which includes the famousSan Andreas Fault of California. Over 600 earthquakes occur in the park each year, helping seismologists to understand this fault system. Most of these earthquakes are too small to be felt, although two large earthquakes did occur in 2002. On October 23, 2002, a magnitude 6.7 earthquake occurred in the park, and on November 3, 2002, amagnitude 7.9 earthquake occurred. These earthquakes did not cause a significant loss of life or property, since the area is very sparsely populated, but they did trigger thousands of landslides.[35]
Glaciers cover about 16% of the 6 million acres of Denali National Park and Preserve. Measurements indicate thatglaciers in the park are losing about 6.6 ft (2 m) of vertical water equivalency each year.[36] There are more extensive glaciers on the southeastern side of the range because more snow is dropped on this side from the moisture-bearing winds from theGulf of Alaska. The 5 largest south-facing glaciers areYentna (20 miles (32 km) long),Kahiltna (30 miles (48 km)),Tokositna (23 miles (37 km)),Ruth (31 miles (50 km)), andEldrige (30 miles (48 km)).[33] The Ruth glacier is 3,800 ft (1,200 m) thick.[35] However, the largest glacier,Muldrow Glacier (32 miles (51 km) long), is located on the north side. Nonetheless, the northern side has smaller and shorter glaciers overall. Muldrow glacier has"surged" twice in the last hundred years. Surging means that it has moved forward for a short time at greatly increased speed, due to a build-up of water between the bottom of the glacier and the bedrock channel floating on the ice (due to hydrostatic pressure).[33]
At the upper ends of Denali's glaciers are steep-walled semicircular basins calledcirques. Cirques form from freeze-thaw cycles of meltwater in the rocks above the glacier and glacial erosion and mass wasting occur under the glacier. As cirques on the opposite sides of a ridge are cut deeper into the divide, they form a narrow, sharp, serrated ridge called anarête. As the arête wears away from glacial ice erosion, the low point between cirques is called acol (or if it is large a pass). Cols are saddle-shaped depressions in the ridge between cirques. A spire-like sharp peak, thehorn, forms when cirques cut back into a mountaintop from three or four sides.
Glaciers deposit rock fragments, but the most notable of the depositions are theerratics, which are large rock fragments carried some distance from the source, found on glacial terraces and ridge tops in many places throughout Denali. Headquarter erratics are made of granite and can be the size of a house. Some erratics (like those from the Yanert Valley) are located 30 miles (48 km) away from their original location.
Large amounts of rock debris are carried on, in, and beneath the ice as the glaciers move downslope. Lateralmoraines are created as debris accumulates as low ridges of till that ride along the edge of the moving glaciers. When lateral moraines adjacent to each other join, they create medial moraines, which are also carried down on the surface of the moving ice.
Braided meltwater streams heavily loaded with rock debris continually shift and intertwine their channels over valley floors. Valley trains are built up as streams drop quantities of poorly sorted sediment. Valley trains are long, narrow accumulations of glacial outwash, confined by valley walls.
Kettles are formed when glacial retreat and melting is rapid, and blocks of ice are still buried undertill. When the ice under the till melts, the till slumps in and forms depressions called kettles. When kettles fill with water, they are known as kettle lakes. Kettle lakes are visible near the Polychrome Overlook, the Teklanika rest stop, and Wonder Lake.[37]: 45
Permanently frozen ground is known aspermafrost. The permafrost is discontinuous in Denali due to differences in vegetation, temperatures, snow cover, and hydrology.[38] The active layer freezing and thawing seasonally can be from 1 inch (25 mm) to 10 feet (3.0 m) thick. The permafrost layer is located between 30 and 100 feet (9.1 and 30.5 m) below the active layer. A stand of oddly leaning white spruce growing on a lower slope of Denali is called theDrunken Forest. The trees lean due to the soil sliding as a result of permafrost freeze/thaw cycles. Permafrost impacts the ecosystem in the park by influencing hydrology, patterns of vegetation, and wildlife.[39] During the very coldPleistocene climates, all of Denali was solidly frozen.[40] The northern areas of the range are still frozen due to continued cold temperatures. About 75% of Denali had near-surface permafrost, or an active permafrost layer, in the 1950s.[41] In the 2000s, around 50% of Denali had near-surface permafrost. It is suspected that by the 2050s, only about 6% of surface permafrost will remain.[40] Because of climate change, most of the shallow permafrost is thawing. It is estimated that with an additional 1–2 degree warming, most of Denali's permafrost will thaw.[42] Permafrost thaw causes landslides as the ice-rich soil transforms into mud slurry.[43] Landslides have previously impacted accessibility in Denali by obstructing the roads in the park.[44] Permafrost thaw releases additional carbon into the atmosphere.[45]
Shallow ponds in Denali are known asthaw lakes and cave-in lakes that are formed when the water warmed by the sun forms basins in the underlying permafrost. These ponds deepen gradually during the summer and, if the temperature is high enough, they will grow in size as their rims collapse.
Thermal expansion and contraction causes permafrost cracking. In the summer water fills these cracks and forms veins calledice wedges. These wedges enlarge with seasonal freezing/thawing cycles. Some ice wedges buried for centuries are revealed during excavations or landslides.
According to theKöppen climate classification, Denali National Park has asubarctic climate (Dfc). Theplant hardiness zone at Denali Visitor Center is 3a with an average annual extreme minimum temperature of −38.9 °F (−39.4 °C).[47]
Long winters are followed by short growing seasons. Eighty percent of the bird population returns after cold months, raising their young. Most mammals and other wildlife in the park spend the brief summer months preparing for winter and raising their young.
Summers are usually cool and damp, but temperatures in the 70s are not rare. The weather is so unpredictable that there have even been instances of snow in August.
The north and south side of the Alaskan Range have completely different climates. TheGulf of Alaska carries moisture to the south side, but the mountains block water to the north side. This brings a drier climate and huge temperature fluctuations to the north. The south has transitional maritime continental climates, with moister, cooler summers, and warmer winters.
| Climate data for McKinley Park, Alaska, 1991–2020 normals, extremes 1923–present | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Record high °F (°C) | 52 (11) | 52 (11) | 56 (13) | 67 (19) | 81 (27) | 91 (33) | 88 (31) | 88 (31) | 82 (28) | 69 (21) | 56 (13) | 52 (11) | 91 (33) |
| Mean maximum °F (°C) | 38.6 (3.7) | 41.1 (5.1) | 41.9 (5.5) | 55.1 (12.8) | 70.5 (21.4) | 79.7 (26.5) | 80.0 (26.7) | 75.7 (24.3) | 64.0 (17.8) | 52.1 (11.2) | 38.2 (3.4) | 38.3 (3.5) | 82.6 (28.1) |
| Mean daily maximum °F (°C) | 10.1 (−12.2) | 19.6 (−6.9) | 25.1 (−3.8) | 40.6 (4.8) | 54.9 (12.7) | 65.3 (18.5) | 66.4 (19.1) | 61.1 (16.2) | 50.7 (10.4) | 33.7 (0.9) | 17.6 (−8.0) | 13.8 (−10.1) | 38.2 (3.5) |
| Daily mean °F (°C) | 2.2 (−16.6) | 9.3 (−12.6) | 12.5 (−10.8) | 28.7 (−1.8) | 43.0 (6.1) | 53.0 (11.7) | 55.5 (13.1) | 50.9 (10.5) | 40.8 (4.9) | 24.7 (−4.1) | 9.8 (−12.3) | 5.6 (−14.7) | 28.0 (−2.2) |
| Mean daily minimum °F (°C) | −5.7 (−20.9) | −0.9 (−18.3) | −0.1 (−17.8) | 16.9 (−8.4) | 31.1 (−0.5) | 40.8 (4.9) | 44.5 (6.9) | 40.8 (4.9) | 30.9 (−0.6) | 15.7 (−9.1) | 1.9 (−16.7) | −2.5 (−19.2) | 17.8 (−7.9) |
| Mean minimum °F (°C) | −33.5 (−36.4) | −27.1 (−32.8) | −21.9 (−29.9) | −3.9 (−19.9) | 19.3 (−7.1) | 31.4 (−0.3) | 35.8 (2.1) | 29.8 (−1.2) | 16.1 (−8.8) | −3.0 (−19.4) | −18.5 (−28.1) | −26.2 (−32.3) | −36.2 (−37.9) |
| Record low °F (°C) | −52 (−47) | −54 (−48) | −47 (−44) | −33 (−36) | −14 (−26) | 19 (−7) | 23 (−5) | 17 (−8) | −6 (−21) | −24 (−31) | −37 (−38) | −54 (−48) | −54 (−48) |
| Averageprecipitation inches (mm) | 0.61 (15) | 0.71 (18) | 0.51 (13) | 0.43 (11) | 0.84 (21) | 2.42 (61) | 3.12 (79) | 3.01 (76) | 1.74 (44) | 0.84 (21) | 0.84 (21) | 0.83 (21) | 15.90 (404) |
| Average snowfall inches (cm) | 9.6 (24) | 9.6 (24) | 8.2 (21) | 6.9 (18) | 2.6 (6.6) | 0.1 (0.25) | 0.0 (0.0) | 0.0 (0.0) | 5.0 (13) | 9.4 (24) | 12.9 (33) | 12.4 (31) | 76.7 (194.85) |
| Average precipitation days(≥ 0.01 in) | 7.6 | 6.0 | 4.9 | 4.0 | 6.5 | 12.6 | 15.6 | 15.6 | 11.8 | 9.7 | 9.8 | 9.3 | 113.4 |
| Average snowy days(≥ 0.1 in) | 9.1 | 7.3 | 6.2 | 4.6 | 1.7 | 0.0 | 0.0 | 0.7 | 2.1 | 8.3 | 11.4 | 10.5 | 61.9 |
| Source 1: NOAA[48] | |||||||||||||
| Source 2: WRCC (extremes)[49] | |||||||||||||
TheAlaska Range is a mountainous expanse running through the entire park, strongly influencing the park's ecosystems. Vegetation in the park depends on the altitude. Thetreeline is at 2,500 ft (760 m), causing most of the park to be a vast expanse oftundra. In the lowland areas of the park, such as the western sections surrounding Wonder Lake,spruces andwillows dominate the forest. Most trees and shrubs do not reach full size, due to unfavorable climate and thin soils. There are three types of forest in the park: from lowest to highest, they are low brush bog, bottomland spruce-poplar forest, and upland spruce-hardwood forest. The forest grows in a mosaic, due to periodic fires.
In the tundra of the park, layers of topsoil collect on rotten fragmented rock moved by thousands of years of glacial activity.Mosses,ferns, grasses, andfungi grow on the topsoil. In areas ofmuskeg,tussocks form and may collectalgae. The term 'muskeg' includes spongy waterlogged tussocks as well as deep pools of water covered by solid-looking moss. Wildblueberries andsoap berries thrive in the tundra and provide the bears of Denali with the main part of their diet.
Over 450 species of flowering plants fill the park and can be viewed in bloom throughout summer. Images ofgoldenrod,fireweed,bluebell, andgentian filling the valleys of Denali are often used on postcards and in the artwork.
Denali is home to a variety of North American birds and mammals, including an estimated 300–350grizzly bears on the north side of the Alaska Range (70 bears per 1,000 square miles) and an estimated 2,700black bears (334 per 1,000 square miles). As of 2014[update], park biologists were monitoring about 51wolves in 13 packs (7.4 wolves per 1,000 square miles), while surveys estimated 2,230caribou in 2013, and 1,477moose in 2011.[50]Dall sheep are often seen on mountainsides. Smaller animals such ascoyotes,hoary marmots,shrews,Arctic ground squirrels,beavers,pikas, andsnowshoe hares are seen in abundance.Red andArctic fox species,martens,Canada lynx, andwolverines also inhabit the park but are more rarely seen due to their elusive natures.
Many migratory bird species reside in the park during late spring and summer. There arewaxwings,Arctic warblers,pine grosbeaks, andnorthern wheatears, as well asptarmigan and thetundra swan. Raptors include a variety ofhawks,owls, andgyrfalcons, as well as the abundant but strikinggolden eagles.
Ten species of fish, includingtrout,salmon, andArctic grayling, share the waters of the park. Because many of the rivers and lakes of Denali are fed by glaciers, glacial silt and cold temperatures slow the metabolism of the fish, preventing them from reaching normal sizes.[citation needed] A single amphibious species, thewood frog, also lives among the lakes of the park.
There are several non-native species in the park includingcommon dandelion,narrowleaf hawksbeard,white sweet clover,bird vetch,yellow toadflax, andscentless false mayweed.[51][52] There are 28invasive species documented in the park and 15 of these species are considered a threat.[51] Volunteers and park rangers work to keep non-native plant populations low.[51]
Denali park rangers maintain a constant effort to keep wildlife wild by limiting the interaction between humans and park animals. Feeding any animal is strictly forbidden, as it may cause adverse effects on the feeding habits of the creature. Visitors are encouraged to view animals from safe distances. In August 2012 the park experienced its first known fatal bear attack when a lone hiker apparently startled a large male grizzly while photographing it. Analysis of the scene and the hiker's camera strongly suggest he violated park regulations regarding backcountry bear encounters, which all permit holders are made aware of.[53] Certain areas of the park are often closed due to uncommon wildlife activity, such as denning areas of wolves and bears or recent kill sites.
The park is serviced by the 92 mi (148 km) long Denali Park Road, which begins at the George Parks Highway and continues to the west parallel to theAlaska Range, ending atKantishna. The park road is the sole vehicle access to the park.[54] Only 15 mi (24 km) of the road, up to Savage River Bridge and a loop trail, is paved becausepermafrost and thefreeze-thaw cycle would create a high cost for maintaining a paved road. Private vehicles are restricted beyond this point. Access to the interior of the park is only through tour/shuttle buses.[55][56][57][58]
The road has been impacted by the Pretty Rocks landslide at Polychrome Pass at Mile 45.4. NPS believes the landslide has been active since before the road was built, but only required moderate maintenance every 2–3 years. Beginning in 2014, the landslide accelerated considerably as permafrost thawed, requiring the road crew to spread 100 truckloads of gravel per week to keep the road passable until August 2021, when the park decided to close the road beyond Mile 45 until summer of 2026 at the earliest.[59][60][61]
Located 1 mi (1.6 km) within the park, the Denali Bus Depot sells tickets for bus trips into the park and is the visitor contact station for campgrounds. All shuttle buses depart from here, as do some tours.[62] The Denali Visitor Center is at mile marker 1.5 and features an exhibit hall and ranger-led programs. It is also close to theMurie Science and Learning Center, theDenali National Park railroad depot, and theMcKinley National Park Airport[63] The railroad station offers service for theAlaska Railroad'sDenali Star route between mid-May and Mid-September.[64]
Three campgrounds near the entrance to the park are accessible by private vehicles: Riley Creek, Savage River, and Teklanika River. Camper buses provide transportation to campgrounds in the interior of the park (Sanctuary River, Igloo Creek, andWonder Lake). All shuttle and tour buses make a stop at Toklat River Contact Station at mile 53. Eielson Visitor Center is located four hours into the park on the road (at mile marker 66). It features daily ranger-led programs during the summer, and on clear days, views of Denali and the Alaska Range.[63] Wonder Lake and Kantishna are a six-hour bus ride from the Denali Visitor Center.[65] Snow closes the Park Road past the park headquarters for the winter between October to April, though the park remains open for cross-country skiing, snowshoeing, and dogsledding.[66][67]
Kantishna features backcountry lodges accessible by chartered air taxi flight to theKantishna Airport.[68][69] Lodging, restaurants, and other services are in the community ofDenali Park, one mile north of the park entrance on the George Parks Highway.[70][57]
While the main park road goes through the Denali Wilderness, the national preserve areas, on the northwest and southwest ends of the park, and portions of the park not designatedwilderness are even more inaccessible with no roads. The far north of the park, characterized by hills and rivers, is accessed from the east by theStampede Trail, a dirt road that effectively stops at the park boundary near the former location of theInto the Wild bus.[71] The rugged south portion of the park, characterized by largeglacier-filledcanyons, is accessed by Petersville Road, a dirt road that stops about 5 mi (8.0 km) outside the park.[72] The mountains can be accessed most easily by air taxis that land on the glaciers.[73][74][75]
Visitors who want to climbDenali need to obtain a climbing permit first and go through an orientation at the Walter Harper Talkeetna Ranger Station inTalkeetna, Alaska, about 100 mi (160 km) south of the entrance to Denali National Park and Preserve. This center serves as the center of mountaineering operations.[76][77]
Maintainedhiking trails are at Savage River, Eielson Visitor Center, Wonder Lake, and Riley Creek. The park also encourages off-trail hiking.[78]
Denali has the only sled dog kennel owned by the federal government, wheresled dogs are raised and trained.[79][80] Sled dogs were first used in the park in 1922 to patrol the area to prevent poaching and assist in park development.[81] Park rangers continue to breed theAlaskan huskies for the traditional activity ofmushing and working at the park, particularly during snowy winter. In summer the kennel has dog sledding demonstrations for visitors.[82][79][83] The kennel is part of theMount McKinley National Park Headquarters District, which also includes administration buildings.
{{cite book}}:|work= ignored (help){{cite web}}: CS1 maint: numeric names: authors list (link)
This article incorporatespublic domain material fromDenali National Park, Walter Harper Talkeetna Ranger Station.National Park Service. RetrievedOctober 27, 2021.
Media from Commons
Travel information from Wikivoyage
