Mount Foraker

Mount Foraker

Sunrise on Mt Foraker and Mt Hunter across the Susitna river with fall foliage | Bob Pool

Rising as an immense white massif southwest of Denali, Mount Foraker is the second-highest major summit in the Alaska Range and one of the great glaciated mountains of North America. At 17,400 feet (5,303.5 meters), it towers above the Kahiltna Glacier and an extraordinary wilderness of icefalls, crevasses, sharp ridges, hanging glaciers, and some of the most celebrated technical climbing routes in Alaska.

Foraker is sometimes overshadowed by Denali simply because its neighbor rises nearly 3,000 feet higher. On almost any other landscape, a 17,400-foot mountain with 7,200 feet of topographic prominence would dominate the entire region. Here, it stands across the glacier from North America’s highest mountain.

The comparison can also be misleading. Foraker is not simply a smaller version of Denali. Its established routes are generally more technical, its ridges more committing, and its climbing traffic dramatically lower. The National Park Service has historically recorded only a fraction of the annual attempts seen on Denali.

The mountain is culturally significant as well. Indigenous place-name traditions describe Foraker in relationship with Denali, including Koyukon forms translated as “the tall one’s wife” or simply “the wife.” The Dena’ina name Be’u likewise refers to the mountain as a wife. The familiar climbers’ name Sultana developed from one of these traditions and survives today in the name of the mountain’s long northeast ridge.

Mount Foraker’s English name arrived only in 1899, when U.S. Army lieutenant Joseph Herron named it for Ohio Senator Joseph B. Foraker.

⚡ Fast Facts

Feature	Details
Mountain	Mount Foraker
State	Alaska
Country	United States
Borough	Denali Borough
Protected Area	Denali National Park and Preserve
Wilderness	Denali Wilderness
Mountain Range	Alaska Range
Subrange	Central Alaska Range
Broader Region	Alaska-Yukon Ranges
Elevation	17,400 ft / 5,303.5 m
Prominence	7,200 ft / 2,195 m
Isolation	13.52 mi / 21.75 km
Nearest Higher Terrain	Archdeacons Tower on the Denali massif
Peakbagger Line Parent	Archdeacons Tower
Broader Parent Mountain	Denali
Key Col	Approx. 10,200 ft / 3,109 m
Alaska Range Ranking	2nd-highest major mountain
Major U.S. Elevation Distinction	One of the three highest major mountains associated with the United States
Main Summit	North/Main Summit
Main Summit Elevation	17,400 ft
South Peak	16,812 ft / 5,124 m
Southwest Peak	Approx. 16,500 ft / 5,029 m
Northwest Peak	Approx. 15,030 ft / 4,581 m
Main Rock	Granodiorite and related intrusive rock
Foraker Pluton Age	About 38 million years
Major Tectonic Feature	Denali Fault system
Major Glacier Access	Kahiltna Glacier
Other Nearby Glaciers	Herron, Foraker, Lacuna and Yentna systems
First Main-Summit Ascent	August 6, 1934
First South-Peak Ascent	August 10, 1934
First Ascent Team	Charles Houston, T. Graham Brown and Chychele Waterston
Historic First Route	West Ridge
Southeast Ridge First Ascent	1963
Infinite Spur First Ascent	1977
Sultana Ridge Complete Ascent	1979–1980 winter season
Public Hiking Trail	None
Climbing Permit	Required
Advance Registration	Normally at least 60 days
Character	Remote technical expedition mountain

📍 Where Is Mount Foraker?

Mount Foraker lies in Denali National Park and Preserve in south-central Alaska, approximately 14 miles southwest of Denali.

The mountain rises directly above the enormous Kahiltna Glacier system.

Nearby major summits include:

Denali
Mount Hunter
Mount Crosson
Mount Russell
The Fin
Numerous unnamed peaks, buttresses and glacier divides

Mount Foraker occupies the central Alaska Range, a landscape containing some of North America’s greatest vertical relief.

Although the mountain sits within one of America’s most famous national parks, no road approaches its base.

For most climbers, access begins far away in Talkeetna, followed by a flight in a ski-equipped aircraft to the Kahiltna Glacier.

🏔️ Second-Highest Mountain in the Alaska Range

Mount Foraker is the second-highest major independent mountain in the Alaska Range, behind Denali.

The difference in elevation is dramatic:

Denali — 20,310 ft
Mount Foraker — 17,400 ft
Mount Hunter — approximately 14,573 ft

Foraker therefore stands almost 2,800 feet above Mount Hunter while remaining nearly 3,000 feet below Denali.

Within the United States, only Denali and the international-border summit of Mount Saint Elias are higher among major independent mountains.

📏 How High Is Mount Foraker?

The accepted modern elevation is:

17,400 feet / 5,303.5 meters

Older references sometimes list 17,395 feet or round the metric elevation differently.

The modern USGS topographic figure of 17,400 feet remains the standard value used by Peakbagger and the National Park Service.

Unlike several summits recently refined by LiDAR to tenths of a foot, Foraker’s immense snow- and ice-covered summit remains conventionally mapped to a rounded elevation.

The mountain’s prominence is approximately:

7,200 feet / 2,195 meters

That is enough to place Foraker among the most topographically prominent mountains in the United States.

🧭 Nearest Higher Neighbor

Mount Foraker’s topographic relationship with Denali is slightly more complicated than simply saying “Denali is the nearest higher mountain.”

Peakbagger’s current database calculates Foraker’s nearest higher terrain at Archdeacons Tower, a subsidiary feature on the Denali massif.

It gives:

Isolation: 13.52 mi / 21.75 km
Key col: approximately 10,200 ft
Clean prominence: 7,200 ft
Line parent: Archdeacons Tower

Archdeacons Tower itself is subordinate to Denali.

In broader mountain-parentage terms, therefore, Denali is the dominant higher mountain associated with Foraker.

ListsOfJohn simplifies this hierarchy and directly identifies Denali as Foraker’s parent.

Both approaches describe the same underlying topographic relationship: Foraker stands as a remarkably independent mountain, but Denali is the higher massif controlling its ultimate parentage.

Mt. Foraker above a sea of clouds, lit up by the arctic’s midnight sun, as seen from Denali, Denali National Park, Alaska | Johnathan Esper

🏔️ A Mountain With Several Summits

Mount Foraker is not a simple single cone.

The massif contains several substantial summits and high points.

Main Summit

The recognized principal summit reaches:

17,400 feet

This corresponds to the historically described North Peak reached by the 1934 expedition.

South Peak

The South Peak reaches approximately:

16,812 feet

It has only about 212 feet of independent prominence and is therefore considered a subsidiary summit.

Southwest Peak

A broad southwestern high point reaches approximately:

16,500 feet.

Northwest Peak

The Northwest Peak reaches approximately:

15,030 feet.

These multiple summits help give Mount Foraker its enormous, complicated appearance.

🧭 Why the 1934 Summit History Can Be Confusing

Older mountaineering literature sometimes creates confusion about which of Foraker’s summits was highest.

The first-ascent team itself had limited mapping and no precise modern elevation data.

Charles Houston wrote that when the climbers reached the summit plateau, wind and cloud made it difficult to determine which peak was highest.

They eventually decided that the North Peak was the true summit.

They climbed it on August 6, 1934.

Four days later, after a substantial storm dropped around 30 inches of snow, they returned to climb the South Peak on August 10.

Modern topographic databases support their judgment: the principal northern/main summit is 17,400 feet, while the South Peak is substantially lower at roughly 16,812 feet.

Some modern databases nevertheless use August 10 as the formal first-ascent date, apparently treating the expedition’s completion of both historical summits as the definitive first ascent.

For historical clarity, the best wording is:

Main/North Summit first reached August 6, 1934; South Peak climbed August 10, 1934.

🪶 Indigenous Names and Relationships

Mount Foraker existed within Indigenous cultural landscapes long before the English name appeared on a map.

Modern research into Alaska Native place names records several traditions.

A Koyukon form is rendered as:

Deenaalee Be’ot / Ch’e’ot

with meanings translated as:

“the tall one’s wife” or “the wife.”

Related Lower Tanana and Upper Kuskokwim forms are also recorded.

The Dena’ina name Be’u likewise refers to the mountain as a wife in relationship with Denali.

This family relationship extends to nearby Mount Hunter, known in Dena’ina as Begguya, often translated as “Denali’s child.”

Together, the three mountains form not simply a geographic group but part of a much older cultural landscape.

🪶 What About the Name Sultana?

Sultana is widely associated with Mount Foraker in climbing literature.

The history is more nuanced than simply calling it “the original Native name.”

Modern Alaska Native place-name research records a Koyukon term Solt’aanh, meaning “woman.”

However, researchers note that it was not commonly used as the established mountain place name.

The same research says the climbers’ name Sultana Ridge was based on Koyukon names recorded by earlier writers such as Hudson Stuck and George Byron Gordon.

That means Sultana is best described as an Indigenous-derived historical climbing name, while the more securely documented Native place-name forms include names translated as “the wife” or “the tall one’s wife.”

This distinction is worth preserving rather than flattening several language traditions into one supposedly universal name.

🏷️ Why Is It Called Mount Foraker?

The modern English name dates to 1899.

U.S. Army lieutenant Joseph S. Herron traveled through the region during an expedition attempting to identify a practical route from Cook Inlet toward Interior Alaska.

From the Lake Minchumina region, Herron obtained exceptional views of the great central Alaska Range.

He named the 17,400-foot mountain for Joseph Benson Foraker, then a U.S. senator from Ohio.

Foraker had also served as governor of Ohio.

The name later entered official federal mapping.

As with many Alaska mountains, the English political name was applied to a landscape that already possessed Indigenous names and relationships.

🪨 Geology of Mount Foraker

Mount Foraker is built largely from granodiorite, a strong crystalline intrusive rock closely related to granite.

That geology is critically important.

The tallest mountains of the central Alaska Range tend to coincide with resistant intrusive bodies capable of surviving extremely aggressive glacial erosion.

Mount Foraker is no exception.

Its major intrusive body is known as the Foraker pluton.

Geological dating places the pluton at approximately:

38 million years old

This makes Foraker’s main intrusive rock much younger than many of the ancient metamorphic rocks found elsewhere in Alaska.

🔥 What Is Granodiorite?

Granodiorite forms when magma cools slowly beneath Earth’s surface.

Because cooling occurs underground, mineral crystals have enough time to grow large enough to become visible.

Granodiorite commonly contains:

Quartz
Plagioclase feldspar
Potassium feldspar
Biotite
Hornblende

Chemically, it falls between granite and darker dioritic rocks.

The rock can be exceptionally strong when intact.

This resistance has helped the Foraker massif stand far above the surrounding landscape despite intense glacial erosion.

🌋 An Ancient Magma Chamber

Mount Foraker was not created as a volcano.

The granodiorite forming much of the mountain crystallized deep underground.

Magma intruded surrounding sedimentary and metamorphic rocks and slowly solidified.

Only later did tectonic uplift and erosion expose it.

That means hikers or climbers looking at Foraker’s cliffs are essentially seeing rock that once formed within a deep magmatic system far beneath an earlier landscape.

Millions of years of uplift and erosion removed the material that originally covered it.

🧩 The Foraker and McGonagall Plutons

Mount Foraker contains one of the most fascinating geological markers in Alaska.

USGS geologists discovered that the Foraker pluton and a similar body known as the McGonagall pluton have nearly identical mineralogy and chemistry.

They appear to have once formed one continuous igneous body.

Today, however, the two are separated.

Why?

The Denali Fault moved them apart.

Research indicates approximately 38 kilometers of right-lateral displacement since the granodiorite crystallized.

Mount Foraker therefore contains physical evidence of tens of kilometers of tectonic motion.

⚡ The Denali Fault

The Denali Fault system is one of the great active faults of Alaska.

It stretches for more than a thousand miles through Alaska and western Canada.

The fault accommodates significant horizontal motion as crustal blocks respond to plate convergence in southern Alaska.

The Foraker–McGonagall pluton relationship gives geologists an unusually useful marker for estimating past movement.

If two pieces of once-connected granite now sit dozens of kilometers apart, the offset provides direct evidence of fault displacement.

🌎 Why the Alaska Range Is Rising

The Alaska Range owes its enormous elevation to active tectonic compression.

South of Alaska, the Pacific Plate moves beneath North America.

The Yakutat microplate also collides with southern Alaska.

These interactions compress and thicken the crust.

Fault systems accommodate movement while blocks of rock are pushed upward.

The ancestral Alaska Range began developing during the Cretaceous, but much of the range’s extraordinary modern relief results from comparatively recent Cenozoic uplift.

The mountains are still tectonically active today.

Mount Foraker in Alaska Range, in Denali National Park by Mount McKinley | Justin Beyerlin

🪨 The “Teflon Peaks”

Geologists have sometimes referred to the great granite mountains of the western Alaska Range as “Teflon Peaks.”

The term comes from a scientific study examining why the tallest granite mountains rise so dramatically above the elevation at which glaciers should theoretically erode them down.

Much of the Alaska Range consists of heavily fractured sedimentary rock.

Those areas commonly have local relief of roughly 3,000–5,000 feet.

Intact granitic plutons behave differently.

They resist erosion more effectively.

Denali, Foraker and other granite-dominated mountains can therefore rise thousands of feet above the surrounding glacier network.

Mount Foraker’s extraordinary relief is partly a story about rock strength.

🧊 Glaciers of Mount Foraker

Mount Foraker is surrounded by an immense glacial system.

Major ice bodies around the massif include:

Kahiltna Glacier
Foraker Glacier
Herron Glacier
Lacuna Glacier
Yentna Glacier and its tributaries

Hundreds of smaller hanging glaciers, snowfields and icefalls descend from the mountain’s faces.

These glaciers have carved nearly every major feature of the modern landscape.

🧊 Kahiltna Glacier

The Kahiltna Glacier is the best-known glacier near Mount Foraker.

It flows for roughly 44 miles, making it the longest glacier in Denali National Park and Preserve and the longest in the Alaska Range.

The glacier provides the standard aircraft landing area for Denali climbers.

It also offers access to Mount Foraker, Mount Hunter and numerous smaller technical peaks.

From the Kahiltna, Foraker rises as a colossal wall west of the glacier.

Its scale can be difficult to appreciate from photographs.

The vertical distance from glacier landing zones to the summit approaches 11,000 feet.

🧊 Foraker Glacier

The Foraker Glacier drains part of the mountain toward the northwest and ultimately feeds the Foraker River system.

Early National Park Service descriptions identified it among the major glacier systems originating around the Foraker massif.

Its position on the less frequently visited side of the mountain contributes to the relative isolation of the western and northern approaches.

🧊 Herron Glacier

The Herron Glacier also originates in snowfields around Mount Foraker.

Historic park publications identified it among the largest north-flowing glaciers associated with the central Alaska Range.

The glacier drains toward Interior Alaska rather than the Cook Inlet side of the range.

Mount Foraker therefore contributes ice and meltwater toward fundamentally different drainage systems depending on which side of the mountain receives the snowfall.

🧊 Glacier Erosion

Glaciers continuously alter the mountain.

Ice flows downhill under gravity.

Rock debris frozen into the glacier grinds against bedrock.

Glaciers quarry blocks from fractured slopes.

This process:

Deepens valleys
Widens glacier basins
Sharpens ridges
Steepens cliffs
Produces moraines
Moves enormous quantities of sediment

Where several glaciers erode different sides of a mountain simultaneously, they can create extraordinarily steep pyramidal relief.

Foraker’s great faces are the result of tectonic uplift interacting with millions of years of glacial erosion.

🧊 Crevasses

Glacier travel around Mount Foraker involves extensive crevasse hazard.

Crevasses form where moving glacier ice stretches or flows over uneven terrain.

Some are obvious open chasms.

Others remain hidden beneath snow bridges.

The Kahiltna Glacier landing area itself requires careful management because seasonal melting gradually exposes crevasses.

Higher on Foraker, icefalls, bergschrunds and complex glacier junctions create substantially greater hazards.

Roped glacier travel and crevasse-rescue skills are fundamental to any expedition.

📉 The Kahiltna Glacier Is Losing Mass

Scientific monitoring shows that the Kahiltna Glacier is thinning and losing mass.

Long-term comparisons using photographs, elevation surveys, aircraft measurements and satellite data all show sustained glacier loss.

Warming also affects the seasonal aircraft runway.

As snow melts earlier, hidden glacier crevasses become exposed and the landing surface can become unusable sooner in the season.

These changes have direct consequences for climbers and flightseeing operations as well as the mountain ecosystem.

🏔️ Climate Change and Climbing Routes

Changing glacier conditions can transform routes on Mount Foraker.

As snow and ice thin:

Bergschrunds widen
Crevasses change position
Snow bridges weaken
Rockfall can increase
Ice routes become thinner
Formerly frozen rock becomes unstable
Glacier approaches change

A route description written decades ago cannot be treated as a permanent set of instructions.

The Infinite Spur of 1977, the West Ridge of 1934 and the modern Sultana Ridge all exist within a moving, changing mountain environment.

🌨️ Mount Foraker’s Climate

Weather is one of the mountain’s defining challenges.

Moisture arriving from the Gulf of Alaska produces enormous snowfall across the southern Alaska Range.

Cold Interior air can bring exceptionally low temperatures.

High elevation adds another layer of severity.

Climbers may experience:

Multi-day snowstorms
High winds
Severe cold
Whiteouts
Heavy drifting snow
Rapid warming
Avalanche cycles
Sudden clearing followed by another storm

The mountain’s long ridges provide very little shelter.

A technically straightforward section can become extremely dangerous when wind and visibility deteriorate.

🌬️ Wind

Wind is particularly important on Foraker.

Long ridges accumulate massive snow cornices.

Wind strips some slopes down to hard ice while loading others with unstable snow.

Blowing snow can reduce visibility to only a few feet.

Wind chill at elevations above 15,000 feet can become severe enough to create frostbite quickly.

Early expedition accounts repeatedly describe climbers being pinned down by prolonged storms.

🧗 First Ascent: The 1934 Expedition

Mount Foraker’s first ascent was made by a six-person expedition organized by Charles S. Houston.

The group included:

Charles Houston
T. Graham Brown
Chychele Waterston
Oscar Houston
Charles Storey
Carl Anderson

The team approached through the national park from the north and west rather than flying directly onto the glacier.

The expedition took weeks.

At higher camps, the three summit climbers continued while the remaining members provided essential logistical support.

Houston later emphasized that the climb was effectively a six-person achievement, even though only three members stood on the upper summits.

🧗 August 6, 1934 — Main Summit

Houston, Brown and Waterston reached the summit plateau after difficult climbing through snow, rock and ice.

They initially could not determine which summit was higher because of cloud and blowing snow.

They chose the North Peak.

The route involved roughly 2,500 feet of climbing from the plateau, including steep hard snow and exposed terrain.

They reached the summit on August 6, 1934.

A storm developed rapidly during their descent.

Willow wands placed along the plateau became essential for navigating back through the whiteout.

🌨️ Thirty Inches of Snow

After the main summit climb, the weather collapsed.

The climbers spent several days confined to a tiny high camp.

Roughly 30 inches of new snow accumulated.

Their tent became partially buried.

Food and fuel were limited.

The team knew it would soon have to begin descending.

But they also wanted to climb the second major summit.

August 10 became their final opportunity.

🧗 August 10, 1934 — South Peak

The climbers returned to the plateau and turned toward the South Peak.

Fresh snow made travel much harder.

They sank deeply into unconsolidated snow while approaching a steep ice barrier.

One section required a long delicate traverse below a vertical wall.

The team then climbed an ice chimney between fallen blocks before reaching higher snow.

They stood on the South Peak near sunset on August 10, 1934.

With both summits climbed, the first great exploration of Mount Foraker’s upper mountain was complete.

🧭 The West Ridge

The 1934 expedition reached the upper mountain by what became known as the West Ridge.

Houston considered it the only obvious practical route from the side they had explored.

The climb involved:

Long glacier approaches
Snow ridges
Cornices
Ice
Rock climbing
Severe exposure
Complicated route finding

Despite being the first established route, it did not become an easy or frequently climbed normal route comparable with Denali’s West Buttress.

Mount Foraker has never really developed an “easy” standard route.

🧗 Southeast Ridge — 1963

Foraker was not climbed again until 1963.

Jeffrey Duenwald and James Richardson reached the summit on July 7 by the Southeast Ridge.

The route became the second ascent of the mountain and first ascent of the ridge.

The expedition approached from the Kahiltna side, reflecting the growing importance of glacier aircraft access to Alaska Range climbing.

The Southeast Ridge opened a new chapter in Foraker exploration.

🧗 Northeast Ridge — 1967

A Japanese expedition established another major route in 1967.

The climbers ascended an eastern icefall to reach the northeast ridge.

From there, the route followed a sharp snow ridge before gaining the broader upper mountain.

Three climbers reached the summit on July 7 after ascending nearly 6,000 vertical feet in a single summit day from their high camp.

The descent became difficult in whiteout conditions.

🧗 Archangel Ridge

The mountain’s long northern ridge system was explored through several expeditions.

A major ascent occurred in the 1970s on what became known as Archangel Ridge.

These routes helped establish Foraker’s reputation as a mountain where even ridges can involve enormous horizontal distances and substantial accumulated elevation gain.

Unlike a compact peak where climbing begins almost immediately beneath the summit, some Foraker routes require traversing entire subsidiary mountains and ridge systems before the final ascent begins.

🧗 Sultana Ridge

The famous Sultana Ridge begins with Mount Crosson and then follows an enormous northeast ridge system toward Foraker.

The complete route is approximately 8.5 miles long.

One classic account calculated approximately:

14,072 feet of total climbing
3,672 feet of elevation loss

before the summit is reached.

The final northeast ridge itself rises approximately 5,750 feet.

The technical climbing can be moderate compared with Foraker’s great faces, but the route is extraordinarily exposed to weather.

That combination has made it the closest thing Foraker has to a conventional modern route while remaining a serious expedition.

🏔️ Mount Crosson

Mount Crosson reaches approximately 12,800 feet northeast of Foraker.

On the Sultana Ridge approach, climbers may ascend Crosson before continuing across a succession of saddles and high points toward Foraker.

This produces a psychologically unusual expedition.

Instead of steadily climbing one mountain, teams repeatedly gain and lose elevation over several days.

By the time they reach Foraker itself, they have already completed an enormous mountain journey.

🧗 Infinite Spur

Mount Foraker’s most famous technical route is the Infinite Spur on the South Face.

George Lowe and Michael Kennedy completed its first ascent in 1977.

The climb became one of the landmarks of modern alpine-style mountaineering.

Instead of establishing numerous fixed camps and ropes, Lowe and Kennedy climbed with a lightweight, highly committed approach.

The route contained:

Long sections of approximately 60-degree ice
Rock climbing to about 5.9
Difficult mixed climbing
Enormous exposure
Sustained commitment

They reached the summit on July 3, 1977 and descended via the Southeast Ridge.

🪨 Why the Infinite Spur Matters

The Infinite Spur helped redefine expectations for technical climbing in the greater ranges.

Rather than treating a giant Alaska mountain as a slow siege expedition, Lowe and Kennedy approached it with the speed and technical style associated with smaller alpine climbs.

The route demonstrated that enormous mountain faces could be climbed in committed alpine style.

It remains one of the most respected lines in North American mountaineering.

The climb also illustrates a central truth about Mount Foraker:

Its lower elevation compared with Denali does not make it the easier mountain.

🧗 Winter Ascents

Winter transforms an already severe mountain into an extreme cold-weather environment.

A notable winter ascent occurred in March 2007, when Japanese climber Masatoshi Kuriaki completed a solo winter ascent.

NPS records describe summit conditions around:

−50°F

with winds of:

20–30 knots

producing wind chills approaching −100°F.

Kuriaki had spent years attempting winter climbs in the central Alaska Range.

His ascent demonstrates the extraordinary severity possible on Foraker outside the normal spring mountaineering season.

🥾 Can You Hike Mount Foraker?

No.

Mount Foraker is not a hiking mountain.

There is no maintained trail to its summit.

There is no nontechnical tourist route.

Even the least technically demanding established lines require skills such as:

Glacier travel
Crevasse rescue
Avalanche assessment
Steep snow climbing
Ice climbing
Cornice management
Expedition camping
Severe-weather survival
High-altitude acclimatization
Remote navigation

Technical routes add substantial rock and mixed climbing.

This is a major expedition objective for experienced alpinists.

🎫 Mount Foraker Climbing Permit

Mount Foraker is one of the two mountains in Denali National Park and Preserve subject to the park’s specialized mountaineering registration program.

Climbers must register in advance and receive a Special Use Permit.

For the 2026 season, NPS requires most climbers to register at least:

60 days before the planned start date

Experienced climbers who have physically climbed on Denali or Foraker since 1995 may qualify for a seven-day exception.

Every registered climbing team must also attend a pre-climb orientation at the Walter Harper Talkeetna Ranger Station.

💵 2026 Mountaineering Fee

For 2026, the NPS Mountaineering Special Use Fee is:

$450 per climber
$350 for climbers age 24 or younger

The park entrance fee is separate unless covered by an eligible pass.

Permit fees change over time, so future climbers should always confirm the current amount directly with the National Park Service rather than relying on an older article.

✈️ Flying to the Kahiltna Glacier

Most modern Foraker expeditions begin in Talkeetna.

Ski-equipped aircraft carry climbers toward the Kahiltna Glacier.

Landing depends entirely on conditions.

Cloud, wind, snowfall, glacier melt and visibility can all delay flights.

Climbers must therefore build flexibility into expedition schedules.

Aircraft pickup can also be delayed.

An expedition that finishes its climb may remain on the glacier for days if weather prevents the aircraft from returning.

🏞️ Denali Wilderness

Mount Foraker lies within the Denali Wilderness of Denali National Park and Preserve.

Despite the aircraft access used by climbers, the mountain itself remains an exceptionally undeveloped environment.

There are no permanent summit-route huts.

Climbers must remove gear, food, fuel, wands and waste.

NPS regulations require properly managed caches and prohibit abandoning permanent caches.

The objective is to preserve the high Alaska Range as closely as possible to a self-willed wilderness landscape.

🌿 Flora and Fauna

The summit of Mount Foraker is effectively a polar-alpine environment.

At 17,400 feet there is no conventional vegetation.

Snow, ice, rock, wind and severe cold dominate.

Life becomes much more diverse as elevation decreases toward the tundra and valleys of Denali National Park.

The park contains more than 1,500 documented species of vascular plants, mosses and lichens.

Vegetation ranges from barren glacier and alpine tundra through shrub tundra to spruce woodland and lowland forest.

This habitat supports one of North America’s most complete subarctic wildlife communities.

🌱 Alpine Tundra

Below the permanent snow-and-ice zone, alpine tundra occupies exposed mountain slopes.

Plants must survive:

Cold temperatures
Strong wind
Long snow cover
Short summers
Thin soils
Frost
Extreme seasonal sunlight changes

Typical vegetation includes:

Sedges
Grasses
Dwarf shrubs
Mosses
Lichens
Low flowering plants

Plants remain close to the ground, where temperatures are slightly warmer and wind speeds lower.

🌿 Willow and Dwarf Birch

At somewhat lower elevations, willow and dwarf birch become increasingly common.

These shrubs are ecologically vital.

Moose browse heavily on willow.

Ptarmigan eat buds and shoots.

Birds nest among branches.

Shrubs trap snow, alter soil moisture and provide shelter for small mammals.

As Alaska warms, tall shrubs are expanding into some areas that were previously open alpine tundra, a change scientists are studying closely.

🐏 Dall Sheep

Dall sheep inhabit high mountain terrain throughout parts of Denali.

They favor steep slopes, ridges and rocky terrain where they can escape predators.

Their white coats are particularly striking against dark summer rock.

The protection of Dall sheep was one of the original motivations for establishing Mount McKinley National Park in 1917.

Within the original park boundary, the sheep population remains unusual because it is not hunted and continues living alongside a natural complement of large predators.

🦌 Caribou

Caribou move across tundra, river valleys and mountain passes.

The Denali Caribou Herd spends most of the year north of the Alaska Range and east of the Foraker River.

These animals are exceptionally adapted to long-distance movement.

Their broad hooves function well on snow and soft tundra.

Caribou feed on lichens, sedges, grasses and shrubs.

🫎 Moose

Moose generally occupy lower elevations than Dall sheep.

Willow thickets, rivers, wetlands and boreal forest provide better feeding habitat than the glaciated high mountains.

Even so, the watersheds descending from Foraker ultimately connect the summit environment with extensive moose habitat farther downstream.

An adult Alaska moose can weigh well over 1,000 pounds.

🐻 Grizzly Bears

Grizzly bears roam across Denali’s tundra and river valleys.

Their diet changes seasonally and can include:

Roots
Berries
Grasses
Ground squirrels
Carrion
Other available foods

Bears do not routinely occupy the upper glaciers of Mount Foraker, where almost no food exists.

However, overland approaches and lower-elevation travel within Denali occur in bear habitat.

🐺 Wolves

Gray wolves remain part of the intact predator community of Denali.

They travel across enormous territories while hunting caribou, moose, sheep and smaller animals.

Wolves are difficult to observe because populations occur at relatively low density and packs shift their movements through large areas.

Their continued presence helps make Denali one of the finest large-mammal ecosystems in North America.

🐾 Wolverines

The wolverine may be the animal best matched to the character of the Alaska Range.

Wolverines travel huge distances across tundra, snow and mountain terrain.

They occur at low density but are capable of crossing high passes and glacier systems.

Their broad feet help them move over snow.

They feed opportunistically on carrion and prey.

Remote mountains such as Foraker provide exactly the enormous undeveloped landscapes wolverines require.

🐇 Collared Pikas

Collared pikas inhabit talus slopes at lower elevations around the Alaska Range.

These small relatives of rabbits do not hibernate.

During the brief summer they gather vegetation and store it in haypiles beneath rocks.

The plants provide food during the long winter.

Scientists in Denali are studying collared pikas and other alpine species to understand how warming and changing vegetation may affect their habitat.

🐿️ Hoary Marmots

Hoary marmots occupy rocky slopes and alpine meadows.

They spend summer feeding intensively before entering prolonged winter hibernation.

Their loud alarm whistles can carry long distances.

Marmots are much more likely to occur around vegetated alpine terrain than on Foraker’s glacier-covered upper mountain.

🦅 Golden Eagles

Golden eagles hunt over open tundra and mountains.

They use rising air around ridges to travel efficiently while searching for prey.

Ground squirrels, hares, ptarmigan and other small animals may form part of their diet.

Denali supports extensive open habitat favorable to these large raptors.

🐦 Ptarmigan

Several ptarmigan species occur in Alaska’s mountain environments.

Their seasonal plumage provides excellent camouflage.

Summer feathers blend with tundra and rock.

Winter plumage becomes predominantly white.

Feathered feet provide warmth and help the birds travel across snow.

The birds represent another example of the remarkable adaptations required for life in the Alaska Range.

🌊 A Continental Drainage Divide

Mount Foraker stands along a major hydrological divide.

Different sides of the mountain eventually feed river systems flowing toward very different parts of Alaska.

Southern and southeastern drainage contributes toward the Susitna River and Cook Inlet, ultimately reaching the Gulf of Alaska and Pacific Ocean.

Northern and northwestern drainage contributes toward systems connected with the Tanana and Yukon rivers, ultimately reaching the Bering Sea.

A single storm dropping snow across Foraker can therefore eventually contribute meltwater to opposite sides of Alaska.

🏔️ Mount Foraker vs. Denali

Denali is approximately 2,910 feet higher than Mount Foraker.

Feature	Mount Foraker	Denali
Elevation	17,400 ft	20,310 ft
Prominence	7,200 ft	20,146 ft
Isolation	13.52 mi	More than 4,600 mi
Alaska Range Rank	2nd	1st
First Ascent	1934	1913
Character	Highly technical expedition peak	Enormous high-altitude expedition peak

Denali is vastly more topographically independent.

Foraker, however, can be more technically demanding on established climbing routes.

That is one reason it receives far fewer summit attempts.

🏔️ Mount Foraker vs. Mount Hunter

Mount Hunter rises southeast of the Denali–Foraker massif.

Hunter reaches approximately 14,573 feet, nearly 2,830 feet below Foraker.

Both mountains have formidable technical climbing reputations.

Mount Hunter’s steep faces and corniced ridges have made it an alpine-climbing icon despite its lower elevation.

Foraker combines similar technical seriousness with substantially greater altitude and scale.

🏔️ Mount Foraker vs. Mount Saint Elias

Mount Saint Elias rises to approximately 18,008 feet on the Alaska–Yukon boundary.

That makes Saint Elias higher than Foraker.

Both possess enormous local relief and extensive glacier systems.

Saint Elias rises spectacularly close to the Gulf of Alaska, while Foraker occupies the interior glacial landscape beside Denali.

Their different settings create two of Alaska’s greatest mountain environments.

Mountaineering team ascending the upper Kahiltna Glacier to 11,200 camp, at around midnight, on Denali, Denali National Park, Alaska | Johnathan Esper

💡 Interesting Facts About Mount Foraker

Mount Foraker reaches 17,400 feet (5,303.5 meters).
It is the second-highest major mountain in the Alaska Range.
It has approximately 7,200 feet of clean topographic prominence.
Its true isolation is approximately 13.52 miles.
Peakbagger currently identifies Archdeacons Tower on the Denali massif as its nearest higher terrain and line parent.
In broader mountain terms, Foraker’s dominant higher parent is Denali.
Its key col is approximately 10,200 feet.
The main summit corresponds to the historically described North Peak.
The South Peak reaches approximately 16,812 feet.
Charles Houston, T. Graham Brown and Chychele Waterston reached the main/North Summit on August 6, 1934.
The same three climbers reached the South Peak on August 10, 1934.
The 1934 expedition approached from the north and west rather than landing directly on the Kahiltna Glacier.
Mount Foraker was named in 1899 for Ohio Senator Joseph B. Foraker.
Indigenous names describe the mountain in relationship with Denali as “the wife.”
The Dena’ina name Be’u is associated with Mount Foraker.
Sultana Ridge takes its name from an Indigenous-derived historical climbing name.
Much of Mount Foraker consists of granodiorite.
The Foraker pluton crystallized roughly 38 million years ago.
The Foraker and McGonagall plutons appear to have once been parts of the same intrusive body.
Movement on the Denali Fault displaced them by roughly 38 kilometers.
The Kahiltna Glacier near Foraker is approximately 44 miles long.
The Kahiltna is the longest glacier in Denali National Park and the Alaska Range.
Jeffrey Duenwald and James Richardson completed the second ascent of Foraker by the Southeast Ridge in 1963.
George Lowe and Michael Kennedy first climbed the Infinite Spur in 1977.
The Infinite Spur became a landmark in alpine-style mountaineering.
The Sultana Ridge is approximately 8.5 miles long.
Mount Foraker has no hiking route.
A specialized NPS climbing permit and advance registration are required.
Modern expeditions usually begin with a ski-plane flight from Talkeetna to the Kahiltna Glacier.
Foraker receives dramatically fewer climbing attempts than Denali.
A successful solo winter ascent in 2007 occurred in summit temperatures near −50°F.

🌄 Why Mount Foraker Is Remarkable

Mount Foraker is one of the easiest mountains in North America to underestimate.

It stands beside Denali.

That alone makes comparison almost unfair.

A mountain 17,400 feet high with more than 7,000 feet of prominence would dominate nearly any other landscape on the continent. Beside the highest mountain in North America, Foraker can appear almost secondary.

It is anything but.

Its geological story begins underground.

Roughly 38 million years ago, magma cooled into granodiorite beneath an earlier Alaska landscape. The intrusive body was later broken and displaced by the Denali Fault. Parts of what may once have been the same pluton now lie dozens of kilometers apart.

Tectonic compression continued raising the Alaska Range.

Glaciers attacked the rising mountains.

They excavated valleys, cut immense faces, sharpened ridges and transported extraordinary volumes of rock.

The resistant Foraker granodiorite survived.

It now rises more than 17,000 feet above sea level and roughly 11,000 vertical feet above the Kahiltna Glacier.

The cultural story reaches much farther back than the English name.

Indigenous language traditions understood Foraker in relationship with Denali — as a wife beside the great mountain, while neighboring Mount Hunter formed part of the same family landscape.

The name Mount Foraker arrived in 1899, imposed by an American explorer honoring an Ohio politician who never needed to climb the mountain bearing his name.

Then came mountaineers.

Charles Houston, T. Graham Brown and Chychele Waterston reached the main summit in 1934 after weeks of approach, carrying, storms and route finding. They returned four days later to climb the second major summit after roughly 30 inches of new snow.

For decades, very few people followed them.

Later climbers explored the Southeast Ridge, Northeast Ridge, Archangel Ridge, Sultana Ridge and other lines.

Then, in 1977, George Lowe and Michael Kennedy climbed the Infinite Spur.

Their lightweight alpine-style ascent became one of the defining climbs of its generation.

The mountain continues to change.

The Kahiltna Glacier is losing mass. Crevasses shift. Bergschrunds widen. Snow and ice routes evolve. Climate alters not only the ecosystem but the practical geometry of climbing.

Yet Foraker remains fundamentally wild.

There is no summit trail.

No visitor road.

No lodge.

No guaranteed rescue.

Climbers fly onto a glacier and enter a landscape where storms, avalanches, cold, crevasses, altitude and objective hazard still determine what is possible.

Mount Foraker is not simply Denali’s smaller neighbor.

It is one of the defining mountains of the Alaska Range — geologically extraordinary, culturally layered, heavily glaciated and responsible for some of the most important chapters in North American mountaineering history.

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