Mount Iliamna

Mount Iliamna | Iliamna Volcano

Mount Iliamna, Lake Clark National Park and Preserve, Cook Inlet, Alaska | Danita Delimont

Mount Iliamna, officially known as Iliamna Volcano, is a massive glacier-covered stratovolcano rising to 10,016 feet (3,053 meters) in Alaska’s Chigmit Mountains. Located within Lake Clark National Park and Preserve, the volcano towers above the western shore of Cook Inlet and forms one of the most dramatic mountains visible from portions of the Kenai Peninsula.

Known in Dena’ina as Ch’naqal’in, meaning “one that stands above,” Iliamna is appropriately named. The mountain rises almost directly from near sea level to more than 10,000 feet, while enormous glaciers pour from its summit area in nearly every direction.

Although Iliamna has no confirmed eruption in recorded history, it is an active volcano. Persistent fumaroles release steam and volcanic gases from its upper eastern flank, and the Alaska Volcano Observatory continuously monitors the mountain for changes in seismicity, gas emissions, and other signs of unrest.

Mount Iliamna is also one of Alaska’s most topographically impressive mountains. With approximately 7,816 feet (2,382 meters) of prominence, it qualifies as an ultra-prominent peak and ranks among the most prominent mountains in the United States.

⚑ Fast Facts

FeatureDetails
MountainMount Iliamna / Iliamna Volcano
Dena’ina NameCh’naqal’in
Meaning“One that stands above”
CountryUnited States
StateAlaska
BoroughKenai Peninsula Borough
Mountain RangeChigmit Mountains
Parent RangeAleutian Ranges
Elevation10,016 feet / 3,053 meters
ProminenceApproximately 7,816 feet / 2,382 meters
IsolationApproximately 33.5 miles / 53.92 kilometers
Nearest Higher Neighbor (NHN)Redoubt Volcano
Line ParentRedoubt Volcano
Key ColApproximately 2,200 feet / 671 meters
Mountain TypeActive stratovolcano
Primary Volcanic RockAndesite and associated pyroclastic rocks
CoordinatesApproximately 60.032Β°N, 153.092Β°W
Protected AreaLake Clark National Park and Preserve
Wilderness AreaJay S. Hammond Wilderness
First Recorded AscentJune 4, 1959
First AscensionistsHelga Bading, Erik Barnes, Gregg Erickson, and Paul Crews
Current MonitoringAlaska Volcano Observatory
National Natural LandmarkDesignated 1976

🌎 Where Is Mount Iliamna?

Mount Iliamna rises on the western side of lower Cook Inlet, approximately 136 miles southwest of Anchorage.

It belongs to the Chigmit Mountains, a rugged volcanic range forming the northeastern end of the Aleutian mountain system.

The mountain lies entirely within Lake Clark National Park and Preserve, one of Alaska’s great wilderness landscapes.

Nearby communities include:

  • Pedro Bay
  • Port Alsworth
  • Anchor Point
  • Happy Valley
  • Ninilchik

The mountain is separated from the road system of the Kenai Peninsula by Cook Inlet.

From the east, Iliamna rises spectacularly behind the water, glaciers, forests, tidal flats, and coastal mountains of the western inlet.

The volcano stands south of Redoubt Volcano and west of communities such as Homer and Ninilchik.

Farther north and east are other major Southcentral Alaska peaks including Mount Spurr, Mount Susitna, and Mount Torbert.

πŸ—Ώ Ch’naqal’in: “One That Stands Above”

The Dena’ina name for Mount Iliamna is Ch’naqal’in.

The National Park Service translates the name as “one that stands above.”

It is difficult to imagine a more appropriate description.

From the Cook Inlet coast, Iliamna rises thousands of feet above neighboring terrain in an enormous white pyramid of snow, rock, and glacier ice.

Dena’ina people have lived throughout the Lake Clark and Cook Inlet region for generations, and traditional place names preserve detailed knowledge about landmarks, waterways, travel routes, resources, and cultural relationships with the landscape.

The English-language name also has a long history.

Russian maps published during the 19th century used a form resembling Sopka Ilymna. An earlier Spanish expedition in 1779 apparently referred to the mountain as VolcΓ‘n de Miranda.

Today, Iliamna Volcano is the official name used by the Alaska Volcano Observatory.

πŸ”οΈ Redoubt Volcano: Iliamna’s Nearest Higher Neighbor

Mount Iliamna’s nearest major higher mountain is Redoubt Volcano, located to the north.

Redoubt reaches approximately 10,197 feet, making it only about 180 feet higher than Iliamna.

Peakbagger also identifies Redoubt as Iliamna’s line parent.

The two volcanoes dominate the Chigmit Mountains and form one of Alaska’s great volcanic pairings.

Despite their proximity in elevation, Iliamna has an extraordinary 7,816 feet of clean topographic prominence.

Its key col lies at only about 2,200 feet.

This enormous prominence reflects just how dramatically the volcano rises above the surrounding terrain.

πŸ“ One of Alaska’s Most Prominent Mountains

Mount Iliamna’s prominence places it among an elite group of North American mountains.

A mountain with at least 1,500 meters of topographic prominence is known as an ultra-prominent peak, or simply an Ultra.

Iliamna easily clears that threshold with approximately 2,382 meters of prominence.

Peakbagger ranks Iliamna among:

  • North America’s 2,000-meter-prominence peaks
  • Alaska’s ultra-prominent mountains
  • U.S. mountains with more than 6,000 feet of prominence

Its prominence is greater than that of many much higher mountains.

This is partly because the volcano rises from low terrain close to Cook Inlet rather than being buried among similarly high summits.

Other highly prominent Alaska mountains include Mount Torbert, Mount Marcus Baker, and Mount Hayes.

πŸŒ‹ What Type of Volcano Is Mount Iliamna?

Bears in Lake Clark National Park and Preserve, Alaska, Mount Iliamna | Danita Delimont

Iliamna is a stratovolcano, also called a composite volcano.

Stratovolcanoes form through repeated eruptions that deposit alternating layers of:

  • Lava
  • Volcanic ash
  • Pyroclastic debris
  • Broken volcanic rock

Over time, these materials accumulate into large, steep-sided volcanic mountains.

Iliamna consists principally of andesitic lava flows and pyroclastic rocks.

Its modern appearance has been dramatically modified by glaciers and erosion, so it is not as perfectly symmetrical as some younger stratovolcanoes.

The mountain is broad, deeply dissected, and heavily altered.

Steep headwalls along its southern and eastern sides expose hundreds of meters of volcanic rock, providing natural cross sections through the volcano’s history.

🌏 Why Is Iliamna Volcano Here?

Mount Iliamna belongs to the Alaska-Aleutian volcanic arc, one of the world’s great subduction-zone volcanic systems.

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

As the descending oceanic plate travels deeper into Earth, water and other volatile materials released from it help promote melting in the overlying mantle.

Magma then rises through the crust.

Where enough magma reaches the surface repeatedly, volcanoes develop.

This same tectonic process has produced many of Alaska’s famous volcanoes, including:

  • Iliamna
  • Redoubt
  • Mount Spurr
  • Augustine
  • Katmai
  • Pavlof
  • Shishaldin

The volcanic arc continues southwestward through the Alaska Peninsula and Aleutian Islands.

πŸͺ¨ What Lies Beneath the Volcano?

Iliamna did not begin forming on a blank geological landscape.

The volcano stands on Jurassic-age granitic rocks of the Aleutian Range batholith.

Nearby are even older Jurassic volcanic and sedimentary rocks.

Several kilometers east of the summit lies the important Bruin Bay Fault, which separates major geological units within the region.

Iliamna therefore represents only the youngest major chapter in a geological history extending back well over 100 million years.

Older intrusive rocks formed deep underground before erosion and tectonic processes exposed them.

Much later, repeated volcanic eruptions constructed the modern stratovolcano above this ancient foundation.

πŸ”₯ Is Mount Iliamna Active?

Yes.

Iliamna is classified as an active stratovolcano and is monitored by the Alaska Volcano Observatory.

However, the phrase active does not mean that an eruption is occurring or imminent.

Iliamna has no confirmed eruption in recorded historical observations.

Geological studies nevertheless indicate eruptive activity within the last several centuries, including deposits dated to roughly 300 and 140 years ago.

The volcano also displays persistent geothermal activity.

Perhaps the most obvious evidence comes from its fumaroles.

πŸ’¨ Iliamna’s Fumaroles

Mount Iliamna contains an extensive fumarole field on its upper eastern flank.

Fumaroles are openings through which hot gases and steam escape from underground.

Iliamna’s fumaroles are located at roughly 9,000 feet / 2,740 meters.

Large steam plumes can sometimes rise hundreds of meters above the mountain.

These clouds have repeatedly generated reports of possible eruptions.

Pilots and observers see what appears to be smoke emerging from the volcano, particularly under weather conditions that make condensation especially visible.

In many cases, the apparent eruption turns out to be nothing more than an unusually large steam plume from the persistent fumaroles.

πŸ“‘ Current Volcanic Monitoring

The Alaska Volcano Observatory monitors Iliamna using seismic instruments, satellite observations, webcams, infrasound, and other volcanic monitoring systems.

Periods of increased seismicity have occurred without leading to eruptions.

As of August 2026, the Alaska Volcano Observatory lists Iliamna at:

  • Aviation Color Code: GREEN
  • Volcano Alert Level: NORMAL

Those classifications indicate background or typical non-eruptive conditions.

Because volcanic status can change, anyone relying on current hazard information should always consult the Alaska Volcano Observatory rather than an older article or guidebook.

🧊 The August 2026 Rock and Ice Avalanche

Mount Iliamna’s hazards are not limited to volcanic eruptions.

On August 8, 2026, monitoring instruments detected a large rock and ice avalanche on the volcano’s eastern flank.

The event was recorded by both seismic and infrasound sensors.

The Alaska Volcano Observatory subsequently emphasized that the avalanche did not indicate increased volcanic unrest.

Large avalanches are relatively common on Iliamna.

Similar events have been documented in recent years, including 2016, 2019, and 2023.

This distinction is important because large rock and ice avalanches can produce seismic signals resembling volcanic activity.

🧊 A Mountain Covered in Glaciers

Iliamna is one of Alaska’s great glacier-clad volcanoes.

Most of its upper surface is covered by perennial snow and ice, and approximately ten major glaciers radiate outward from its summit region.

Named glaciers include:

  • Umbrella Glacier
  • Red Glacier
  • Tuxedni Glacier
  • Lateral Glacier
  • Johnson Glacier
  • Tongue Glacier

These enormous bodies of ice are continually moving downhill.

Crevasses open and close, seracs collapse, snow accumulates, and avalanches sweep across the slopes.

From the air, Iliamna can look almost entirely white, with only isolated rock ridges projecting through the ice.

β˜‚οΈ Umbrella Glacier

The Umbrella Glacier lies on the southwest side of the volcano and has played an important role in Iliamna’s climbing history.

It was used during the mountain’s first ascent in 1959.

The glacier has also received enormous deposits from rock and ice avalanches descending from the volcano.

AVO’s geological description specifically notes large avalanche deposits along the Umbrella Glacier.

Climbers traveling here must contend with crevasses, snow bridges, avalanche exposure, and changing glacier conditions.

πŸŸ₯ Red Glacier

The Red Glacier drains the eastern side of Iliamna.

Its position below steep, heavily altered volcanic headwalls places portions of the glacier beneath terrain susceptible to rockfall and avalanches.

The glacier is one of the mountain’s most recognizable features in aerial imagery.

Like glaciers elsewhere in Lake Clark National Park, it responds to changes in snowfall, temperature, and ice dynamics.

πŸ§— First Attempts to Climb Iliamna

Iliamna’s remote location and famously poor weather kept its summit unclimbed well into the 20th century.

Two significant attempts occurred in 1958.

A party consisting of Neil Davis, Pete Isto, Mat Nitsch, Roger Waller, and Keith Hart climbed the southeast side but was forced back by poor weather after reaching approximately 7,500 feet.

Later that summer, Lt. P. J. McEleney led another three-person party onto the northeast face.

They reached roughly 7,000 feet before a severe storm forced them to retreat.

Those attempts demonstrated a recurring theme in Iliamna mountaineering: weather can be a greater obstacle than technical climbing.

πŸ§— First Ascent of Mount Iliamna

The first recorded ascent occurred on June 4, 1959.

The successful team consisted of:

  • Helga Bading
  • Erik Barnes
  • Gregg Erickson
  • Paul Crews

The four were associated with the Mountaineering Club of Alaska.

Their expedition began after they were flown to Chinitna Bay.

From near sea level, they fought through alder, crossed streams, dealt with mosquitoes, and traveled approximately 10 miles inland toward the mountain.

They eventually reached the Umbrella Glacier and established a climbing camp around 3,700 feet.

πŸŒ™ A Nighttime Summit Climb

The first-ascent team took advantage of Alaska’s long early-summer daylight.

They left camp at approximately 6:30 p.m.

Almost the entire climb took place in cloud and poor visibility.

The climbers alternated between:

  • Deep snow
  • Firm crust
  • Glacier travel
  • Crevasse probing
  • Route finding through cloud

Because they expected difficulty navigating back to camp, they left markers along their ascent route.

The team reached Iliamna’s summit at approximately 2 a.m. on June 4, 1959.

Snow was falling, winds were blowing, and visibility remained extremely poor.

Ironically, according to the expedition account, the climbers did not receive their first clear view of the mountain until they were descending from climbing camp.

πŸ₯Ύ Climbing Mount Iliamna Today

Iliamna remains a serious expedition peak.

It does not have a maintained hiking trail, road-accessible trailhead, or standard tourist climbing infrastructure.

Modern parties typically use aircraft to reach glaciers or remote landing sites.

Some expeditions begin relatively high on glaciers, while others attempt a more complete climb from lower elevations.

Routes can involve:

  • Glacier travel
  • Crevasse rescue skills
  • Snow climbing
  • Crampons
  • Ice axe use
  • Rope travel
  • Backcountry skiing
  • Avalanche assessment
  • Navigation in whiteout conditions

A modern ascent should not be confused with simply walking up a snowy volcanic slope.

The combination of glaciers, weather, remoteness, avalanches, and rescue difficulty makes Iliamna a major mountaineering objective.

⛷️ Tuxedni Glacier and West Ridge

A modern approach uses the Tuxedni and Tongue glacier system on the western side of the mountain.

Aircraft may be able to land on suitable glacier terrain when conditions permit.

From glacier camps, climbers can travel upward on skis before transitioning to crampons or snow climbing as the slopes steepen.

The western side provides access toward upper ridges leading toward the summit.

Exact conditions vary enormously from year to year.

Snow depth, glacier crevasses, ice exposure, avalanche debris, weather, and aircraft landing conditions can all determine whether an expedition is practical.

🌨️ Weather

Weather is one of Iliamna’s defining mountaineering challenges.

The volcano rises immediately beside Cook Inlet, exposing it to moisture-rich maritime weather systems.

Conditions may include:

  • Heavy snow
  • Rain at lower elevations
  • Dense fog
  • Strong winds
  • Whiteouts
  • Rapid temperature changes
  • Severe icing
  • Prolonged storms

High precipitation helps maintain Iliamna’s extensive glacier system.

The combination of heavy snowfall and steep upper slopes also contributes to avalanche activity.

Clear weather windows may be short, requiring expedition teams to build substantial flexibility into their plans.

Lake Clark National Park and Preserve, Kachemak Bay, Alaska, aerial landscape and mountains | Danita Delimont

⚠️ Climbing and Volcanic Hazards

Mount Iliamna combines ordinary alpine hazards with hazards specific to an active volcano.

Major risks include:

  • Crevasses
  • Avalanches
  • Serac collapse
  • Rockfall
  • Icefall
  • Whiteouts
  • Strong winds
  • Hypothermia
  • Frostbite
  • Navigation errors
  • Remote rescue conditions
  • Volcanic gases
  • Potential volcanic unrest

The steep, altered rock on portions of Iliamna can be particularly unstable.

Rock-and-ice avalanches are well documented.

Anyone planning an expedition should check both mountain weather and the latest Alaska Volcano Observatory status.

🌊 Lake Clark National Park and Preserve

Mount Iliamna lies within Lake Clark National Park and Preserve, a vast protected landscape containing approximately 2.6 million acres.

The park brings together an extraordinary variety of environments.

These include:

  • Active volcanoes
  • Glaciers
  • Boreal forests
  • Alpine tundra
  • Wild rivers
  • Lakes
  • Coastal salt marshes
  • Tidal flats
  • Rugged mountains

Iliamna and Redoubt Volcano are the park’s two great active stratovolcanoes.

Both were designated National Natural Landmarks in 1976.

Iliamna also lies within the Jay S. Hammond Wilderness, reinforcing the exceptionally undeveloped character of its surroundings.

🌿 Flora and Fauna

Mount Iliamna rises through an extraordinary ecological transition.

Its highest slopes are buried beneath snow and glacier ice, while its lower elevations descend toward some of Alaska’s richest coastal wildlife habitat.

Lake Clark National Park and Preserve contains roughly 800 plant species, dozens of terrestrial mammal species, and nearly 200 recorded bird species.

🌱 Flora

The summit region of Iliamna is essentially devoid of vascular plant life.

Conditions are dominated by:

  • Ice
  • Snow
  • Bare volcanic rock
  • Avalanche debris
  • Extreme wind
  • Freezing temperatures

Vegetation gradually appears lower on the mountain.

The broader coastal side of Lake Clark includes:

  • Alpine tundra
  • Bluejoint meadows
  • Alder thickets
  • Willow
  • White spruce
  • Lutz spruce
  • Mosses
  • Lichens
  • Fireweed
  • Dryas
  • Salmonberry
  • Devil’s club

Freshly exposed glacial terrain undergoes a gradual process of ecological succession.

Mosses and lichens are among the earliest colonizers.

Fireweed, Dryas, willow, and alder eventually establish as soils develop.

At still lower elevations, spruce forest becomes increasingly prominent.

🫐 Coastal and Subalpine Vegetation

The transition from Mount Iliamna toward Cook Inlet is especially dramatic.

Upper mountain environments contain ice and rock.

Lower slopes develop alder thickets and meadow vegetation.

Near the coast are forests, salt marshes, sedge meadows, lagoons, and tidal environments.

This compressed ecological transition is possible because Iliamna rises from near sea level to more than 10,000 feet over a relatively short horizontal distance.

🐻 Brown Bears

The coastal country south and east of Iliamna contains some of Alaska’s most famous brown bear habitat.

Nearby Chinitna Bay is an internationally known bear-viewing destination.

In spring, bears forage in coastal sedge meadows.

Later in the season, changing food availability may draw them toward fish streams, berries, and other resources.

The bears inhabit the lowland landscape below a volcano whose upper reaches are almost completely covered in ice.

Few places better demonstrate the ecological diversity of Southcentral Alaska.

🫎 Other Mammals

Lake Clark National Park and Preserve supports an impressive collection of terrestrial mammals.

Species in the broader region include:

  • Moose
  • Dall sheep
  • Caribou
  • Wolves
  • Brown bears
  • Black bears
  • Wolverines
  • Lynx
  • Red foxes
  • River otters
  • Beavers
  • Snowshoe hares

Not every species regularly occurs on Iliamna’s heavily glaciated slopes.

Most wildlife is concentrated in valleys, coastal areas, forests, tundra, and neighboring mountain terrain where food and shelter are available.

🐟 Salmon

Salmon are essential to Lake Clark’s ecology.

The region contains important habitat for sockeye salmon and other Pacific salmon species.

These fish transport marine nutrients inland when they return from the ocean to spawn.

They support:

  • Brown bears
  • Eagles
  • Other birds
  • Aquatic ecosystems
  • Subsistence communities

Salmon are therefore part of a much larger ecological network connecting the icy mountains around Iliamna with Cook Inlet and the North Pacific.

πŸ¦… Birds

The tremendous variety of habitats around Lake Clark supports a correspondingly diverse bird community.

The park has recorded around 187 bird species.

These include combinations of:

  • Bald eagles
  • Golden eagles
  • Waterfowl
  • Shorebirds
  • Seabirds
  • Ravens
  • Ptarmigan
  • Songbirds
  • Migratory species

Coastal marshes and lagoons are particularly important to waterfowl and migratory birds.

Alpine species occupy much harsher environments farther uphill.

🦭 Marine Wildlife

The ecosystems below Iliamna continue beyond the shoreline.

Cook Inlet and nearby coastal waters support marine mammals including:

  • Harbor seals
  • Sea otters
  • Harbor porpoises
  • Steller sea lions
  • Beluga whales

This creates an extraordinary vertical landscape.

Within a relatively short distance, the environment changes from marine habitat near sea level to salt marsh, spruce forest, alpine tundra, glacier ice, fumaroles, and a 10,016-foot volcanic summit.

🧊 Fire and Ice

Few mountains illustrate the relationship between volcanism and glaciation as dramatically as Iliamna.

Heat remains beneath the volcano.

Steam and volcanic gases escape through fumaroles.

At the same time, enormous quantities of snow and ice cover most of its surface.

These two systems can interact dangerously.

During future eruptive activity, volcanic heat could rapidly melt snow and ice.

Such melting could generate:

  • Lahars
  • Floods
  • Debris flows
  • Ice avalanches

Redoubt Volcano has demonstrated these hazards during modern eruptions.

Iliamna’s extensive glacier cover means similar processes must be included in volcanic hazard planning.

🏞️ A National Natural Landmark

Mount Iliamna was designated a National Natural Landmark in 1976.

The National Natural Landmarks program recognizes exceptional examples of America’s natural heritage.

Iliamna’s combination of active volcanism, extensive glaciers, enormous relief, geological importance, and spectacular landscape makes it an obvious candidate.

The designation occurred in the same year as nearby Redoubt Volcano.

Today, both mountains remain defining natural features of Lake Clark National Park and Preserve.

🌎 Nearby Mountains

Redoubt Volcano

Redoubt Volcano lies north of Iliamna and reaches approximately 10,197 feet.

It is Iliamna’s nearest higher neighbor and line parent.

Unlike Iliamna, Redoubt has produced several well-documented historical eruptions, including major eruptive episodes in 1989–1990 and 2009.

Mount Spurr

Mount Spurr rises farther northeast within the volcanic mountains west of Cook Inlet.

It is another active stratovolcanic system monitored by the Alaska Volcano Observatory.

Mount Torbert

Mount Torbert is the highest summit of the Tordrillo Mountains and one of Southcentral Alaska’s great high-prominence peaks.

Mount Susitna

Mount Susitna rises much closer to Anchorage. Unlike Iliamna, it is not an active volcano.

Mount Marcus Baker

Farther east, Mount Marcus Baker is the highest mountain of the Chugach Range.

πŸ’‘ Interesting Facts About Mount Iliamna

  • Mount Iliamna reaches 10,016 feet (3,053 meters).
  • Its official name is Iliamna Volcano.
  • Its Dena’ina name is Ch’naqal’in, meaning “one that stands above.”
  • Iliamna belongs to the Chigmit Mountains of Alaska’s Aleutian Ranges.
  • The volcano lies within Lake Clark National Park and Preserve.
  • It is an active stratovolcano.
  • Iliamna has no confirmed eruption in recorded history, although geological evidence indicates relatively recent eruptions.
  • Persistent fumaroles regularly produce visible steam plumes.
  • Most of the mountain is covered by permanent snow and ice.
  • Roughly ten glaciers radiate from the volcano.
  • Iliamna has approximately 7,816 feet of topographic prominence.
  • It is an ultra-prominent mountain.
  • Its nearest higher neighbor and line parent is Redoubt Volcano.
  • The first recorded ascent occurred on June 4, 1959.
  • Helga Bading, Erik Barnes, Gregg Erickson, and Paul Crews completed that ascent.
  • Large rock and ice avalanches periodically occur on the volcano.
  • A major avalanche occurred on August 8, 2026, without evidence of increased volcanic unrest.
  • Iliamna became a National Natural Landmark in 1976.
  • Nearby Chinitna Bay supports exceptional brown bear habitat.
  • The mountain rises from ecosystems ranging from coastal wetlands and spruce forest to alpine tundra and permanent glacier ice.

❓ Frequently Asked Questions

How high is Mount Iliamna?

Mount Iliamna reaches 10,016 feet (3,053 meters).

Where is Mount Iliamna?

The volcano lies in Lake Clark National Park and Preserve in Alaska, on the western side of lower Cook Inlet approximately 136 miles southwest of Anchorage.

What mountain range is Mount Iliamna in?

Iliamna belongs to the Chigmit Mountains, part of the Aleutian Ranges.

What is the Dena’ina name for Mount Iliamna?

The Dena’ina name is Ch’naqal’in, meaning “one that stands above.”

Is Mount Iliamna an active volcano?

Yes. Iliamna is an active stratovolcano monitored by the Alaska Volcano Observatory.

When did Mount Iliamna last erupt?

There is no confirmed eruption in recorded history. Geological evidence indicates eruptions occurred within the last several centuries, however, and the mountain retains active fumaroles.

Why does steam come from Mount Iliamna?

A fumarole field on Iliamna’s upper eastern flank releases hot volcanic gases and steam. Under certain weather conditions, the resulting plume can become large enough to resemble an eruption cloud.

What is Mount Iliamna’s nearest higher neighbor?

Its nearest major higher mountain is Redoubt Volcano, which reaches approximately 10,197 feet. Redoubt is also Iliamna’s line parent.

How prominent is Mount Iliamna?

Iliamna has approximately 7,816 feet (2,382 meters) of topographic prominence, making it an ultra-prominent peak.

When was Mount Iliamna first climbed?

The first recorded ascent was completed on June 4, 1959, by Helga Bading, Erik Barnes, Gregg Erickson, and Paul Crews.

Can you climb Mount Iliamna?

Yes, but Iliamna is a remote technical mountaineering objective involving glacier travel, crevasses, snow, avalanche exposure, severe weather, and difficult access. Most expeditions rely on aircraft or lengthy wilderness approaches.

Does Mount Iliamna have glaciers?

Yes. Roughly ten glaciers radiate from its summit region, including Umbrella, Red, Tuxedni, Lateral, Johnson, and Tongue glaciers.

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