Mount Saint Elias

Towering above the glaciers and coastal lowlands of Alaska and Yukon, Mount Saint Elias is one of the most dramatic mountains in North America. Its summit reaches 18,008 feet (5,489 meters) along the international boundary between the United States and Canada, making it the second-highest mountain in both countries.
Only Mount Logan rises higher in Canada, while only Denali rises higher in the United States. Across North America as a whole, Mount Saint Elias ranks fourth in elevation.
What makes the mountain especially remarkable is not just its height but its extraordinary relief. The summit rises only a short distance inland from Icy Bay and the Gulf of Alaska, creating an enormous transition from coastal terrain to an 18,000-foot summit in a relatively small horizontal distance.
Steep glaciers, frequent storms, avalanche hazards, and extreme remoteness have also made Mount Saint Elias one of the great expedition mountains of Alaska and Yukon.
β‘ Fast Facts
| Feature | Details |
|---|---|
| Countries | United States and Canada |
| State/Territory | Alaska / Yukon |
| Mountain Range | Saint Elias Mountains |
| Protected Areas | Wrangell-St. Elias National Park and Preserve / Kluane National Park and Reserve |
| Elevation | 18,008 ft / 5,489 m |
| Prominence | About 11,184 ft / 3,409 m |
| Isolation | About 25.4 mi / 40.8 km |
| Parent Peak | Mount Logan |
| Nearest Higher Neighbor (NHN) | Unnamed Peak on the Mount Logan massif |
| Coordinates | 60.2922Β° N, 140.9314Β° W |
| Boundary Designation | Boundary Peak 186 |
| Tlingit Name | Was’eitushaa |
| First Ascent | July 31, 1897 |
| First-Ascent Expedition Leader | Luigi Amedeo, Duke of the Abruzzi |
| Notable Distinction | Second-highest mountain in both the United States and Canada |
πΊοΈ Where Is Mount Saint Elias?
Mount Saint Elias stands directly on the AlaskaβYukon international boundary.
Its American slopes lie within Wrangell-St. Elias National Park and Preserve, while its Canadian side belongs to Kluane National Park and Reserve.
Both parks form part of a vast transboundary protected landscape containing some of the largest non-polar icefields and highest mountains on Earth.
Unlike Mount Logan, which lies deep within the interior of the Saint Elias Mountains, Mount Saint Elias rises remarkably close to the Gulf of Alaska.
Icy Bay lies immediately to the south, while Yakutat is located farther southeast along the coast.
This proximity to the ocean gives the mountain exceptional vertical relief and contributes to its notoriously stormy weather.
π§ Nearest Higher Neighbor: Unnamed Peak
Mount Saint Elias’s Nearest Higher Neighbor is an Unnamed Peak on the Mount Logan massif, roughly 25 miles northeast.
This higher point reaches approximately 5,633 meters and forms part of the vast Logan summit complex.
Although the immediate NHN is an unnamed summit, Mount Logan itself is Mount Saint Elias’s parent peak.
That relationship makes geographic sense. Mount Logan towers to 19,550 feet only about 26 miles northeast of Saint Elias.
Mount Saint Elias nevertheless possesses extraordinary independence of its own. With more than 11,000 feet of topographic prominence, it ranks among the most prominent mountains in North America.
ποΈ Second-Highest Mountain in the United States and Canada
Mount Saint Elias occupies an unusual place in North American mountain rankings because its summit lies directly on an international border.
At 18,008 feet, it is:
- The second-highest mountain in the United States, after Denali
- The second-highest mountain in Canada, after Mount Logan
- The fourth-highest mountain in North America
- One of the continent’s great ultra-prominent peaks
Its elevation places it above nearly every mountain in Alaska, including Mount Foraker, Mount Bona, Mount Blackburn, and Mount Sanford.
Yet Mount Saint Elias’s elevation tells only part of the story.
Its steep rise from terrain close to sea level makes its profile particularly imposing.
π An Extraordinary Rise from the Sea
Few mountains of comparable height stand as close to an ocean as Mount Saint Elias.
The summit rises approximately 18,000 feet above the coastal landscape surrounding Icy Bay within a horizontal distance of only a few tens of kilometers.
The result is one of the greatest combinations of elevation and local relief anywhere on Earth.
From coastal viewpoints, the mountain does not appear as a distant high plateau. Instead, enormous glaciated slopes rise almost directly behind the coastline.
This steep transition also creates a remarkable range of environments.
Near sea level, visitors encounter temperate rainforest, wetlands, coastal estuaries, and marine ecosystems.
Travel upward and those environments rapidly give way to alpine tundra, bare rock, glaciers, and eventually the permanent snow and ice of the summit.
πͺ¨ Geology of Mount Saint Elias
Mount Saint Elias is not a volcano.
That distinction is worth making because nearby Mount Wrangell, Mount Sanford, Mount Bona, and several other major peaks in eastern Alaska have volcanic origins.
Mount Saint Elias instead owes its enormous elevation primarily to tectonic uplift.
The Saint Elias Mountains occupy one of the most geologically active portions of North America.
A large crustal fragment known as the Yakutat terrane is colliding with and being forced beneath the southern margin of Alaska.
This ongoing collision compresses and thickens the crust, helping drive the rapid uplift of the Saint Elias Mountains.
Earthquakes, faulting, uplift, erosion, and glacial activity continue to reshape the range.
π The Yakutat Terrane Collision
The geology surrounding Mount Saint Elias is particularly fascinating because the mountain range is still actively growing.
The Yakutat terrane was transported northward over millions of years by plate motion.
Today, it is being forced against and beneath other crustal blocks along southern Alaska.
That collision has produced tremendous compression.
Rock layers have been folded, fractured, uplifted, and stacked against one another, creating mountains of exceptional height.
At the same time, glaciers and rivers relentlessly erode those rising mountains.
Mount Saint Elias therefore exists within a geological tug-of-war: tectonic processes push the landscape upward while glaciers, landslides, rivers, and weather tear it down.
π§ A Landscape Dominated by Ice
Glaciers are among the defining features of Mount Saint Elias.
The mountain receives enormous amounts of snow because moisture-laden Pacific storms repeatedly strike the Saint Elias Mountains.
At high elevations, much of this snow survives the summer.
Over time it becomes compressed into glacier ice.
The Mount Saint Elias region connects with a vast network of glaciers and icefields that includes the Seward Glacier, Newton Glacier, Tyndall Glacier, Malaspina Glacier, and numerous smaller ice streams.
Some of these glaciers played central roles in the history of climbing the mountain.
The huge Malaspina Glacier, near the coast, is one of the largest piedmont glaciers in North America.
π§οΈ Why the Weather Is So Severe
Mount Saint Elias has a reputation for prolonged periods of poor weather.
Its coastal position is largely responsible.
Moist air moving inland from the Gulf of Alaska collides with the Saint Elias Mountains and is forced rapidly upward.
As the air rises, it cools and releases moisture as rain or snow.
The result can be:
- Heavy snowfall
- Powerful winds
- Whiteout conditions
- Dense cloud
- Rapidly changing temperatures
- Avalanche-producing storms
- Long periods with little visibility
High elevation adds another layer of difficulty.
Conditions near 18,000 feet can be bitterly cold even when the coastline below is experiencing comparatively mild weather.
These weather patterns are a major reason Mount Saint Elias sees far fewer successful climbs than its fame and elevation might suggest.
π The Name Mount Saint Elias
The English name is associated with the 1741 expedition of explorer Vitus Bering.
Bering sighted the immense mountains of Alaska during his voyage across the North Pacific.
The landform he observed around the feast day of Saint Elias was associated with that saint’s name, and the designation eventually became attached to Mount Saint Elias and the surrounding range.
The mountain is also officially numbered Boundary Peak 186, one of a sequence of summits used in defining sections of the international boundary between Alaska and Canada.
Long before European mapping, however, the mountain already held profound cultural importance for Indigenous peoples of the region.

πͺΆ Was’eitushaa and the Yakutat Tlingit
The Tlingit name commonly recorded for Mount Saint Elias is Was’eitushaa, meaning approximately “mountain at the head of Icy Bay” or “mountain inland of Was’ei.”
Was’ei is a Tlingit name associated with Icy Bay.
For the Yakutat Tlingit, Mount Saint Elias is far more than a geographic landmark.
It is a culturally and spiritually important place connected with traditional stories, clan history, navigation, weather knowledge, songs, and identity.
Tlingit oral traditions describe the mountain as a guide through the immense landscape of glaciers and mountains.
The mountain has also historically been observed for clues about changing weather.
Cloud formations around the summit could signal approaching storms or shifts in wind.
This cultural relationship extends across generations and remains part of the living heritage of the Yakutat Tlingit today.
π§ Early Attempts to Climb Mount Saint Elias
During the late 19th century, Mount Saint Elias became one of the most sought-after summits in North America.
Several expeditions attempted the mountain before anyone reached the top.
Early climbers encountered enormous logistical problems.
Simply reaching the mountain required traveling through coastal wilderness, crossing glaciers, moving heavy supplies, and navigating terrain that was still incompletely mapped.
Expeditions also had little of the lightweight clothing, modern tents, satellite weather forecasts, aircraft support, GPS navigation, and specialized glacier equipment available to climbers today.
Success finally came in 1897.
π§ The First Ascent
The first successful ascent of Mount Saint Elias was made by an Italian expedition led by Luigi Amedeo, Duke of the Abruzzi.
The expedition reached Alaska in the summer of 1897.
Among its members was renowned mountain photographer Vittorio Sella, whose photographs created an extraordinary visual record of the journey.
The expedition began near the coast and transported thousands of pounds of supplies across glaciers.
Progress was exhausting.
Sleds broke under heavy loads, snow bridges crossed hidden crevasses, storms slowed travel, and supplies had to be moved repeatedly between camps.
The climbers traveled across portions of the Malaspina, Seward, Hitchcock, and Newton glacier systems before reaching Russell Col.
Late on July 30, the summit party departed its high camp.
After climbing through the night and morning, the group reached the summit shortly after 11 a.m. on July 31, 1897.
The achievement became one of the landmark ascents of the early era of North American mountaineering.
ποΈ The Abruzzi Ridge
The historic first-ascent route became known as the Abruzzi Ridge.
It approaches Mount Saint Elias from the northern, Yukon side and is one of the famous classic routes in North American mountaineering history.
The route is historically significant but should not be regarded as a straightforward modern climbing option.
Glaciers evolve constantly.
Icefalls move, crevasses expand, snow bridges disappear, and avalanche exposure can change dramatically over time.
A route that worked for an expedition decades ago may present very different hazards today.
Modern climbers therefore need current conditions and route information rather than relying solely on historic descriptions.
π§ββοΈ The Second Ascent
Remarkably, Mount Saint Elias was not climbed again until 1946.
A Harvard Mountaineering Club expedition made the second ascent using a route on the Southwest Ridge.
The long gap between the first and second ascents illustrates just how formidable the mountain remained.
Even as climbing equipment and expedition logistics improved during the first half of the 20th century, Mount Saint Elias continued to demand enormous commitment.
Additional routes were eventually established on the Northwest Ridge, East Ridge, and other parts of the massif.
Many remain major expedition climbs.
βοΈ Winter Climbing
Mount Saint Elias becomes even more formidable in winter.
A winter ascent involves short daylight hours, extreme cold, storms, avalanche danger, crevassed glaciers, and complicated access.
A notable winter ascent was completed in 1996 by David Briggs, Gardner Heaton, and Joe Reichert using the Southwest Ridge area.
The team approached from the Tyndall Glacier and used a variation known as the Milk Bowl to avoid dangerous loose terrain.
Winter climbing on Saint Elias remains an objective for highly experienced expedition mountaineers rather than ordinary recreational climbers.
πΏ Skiing Mount Saint Elias
The mountain’s extraordinary relief has also attracted elite ski mountaineers.
Descending from the upper mountain toward terrain near sea level presents the possibility of one of the largest skiable vertical drops in the world.
But skiing Mount Saint Elias is vastly different from resort skiing or even conventional backcountry skiing.
The terrain includes crevasses, avalanche slopes, ice, seracs, steep glacier sections, severe weather, and huge route-finding challenges.
Only highly accomplished expedition ski mountaineers should contemplate such an undertaking.
π₯Ύ Climbing Mount Saint Elias Today
Mount Saint Elias remains a serious expedition mountain with no easy route.
Teams must be capable of operating independently in remote glaciated terrain for extended periods.
Important skills include:
- Roped glacier travel
- Crevasse rescue
- Snow and ice climbing
- Avalanche assessment
- Cold-weather camping
- High-altitude acclimatization
- Navigation during whiteouts
- Expedition logistics
- Self-rescue
- Weather interpretation
Aircraft access may simplify parts of the approach, but it creates additional uncertainty because poor weather can prevent flights for days.
Teams need enough food, fuel, and equipment to remain self-sufficient if extraction is delayed.
π Permits and Border Considerations
The mountain’s position on the international border adds unusual logistical considerations.
Climbers operating on the Canadian side within Kluane National Park and Reserve must obtain the required mountaineering permits.
Parks Canada requires climbers spending time in Kluane’s Icefield Ranges to register and obtain a mountaineering permit. Aircraft landings within the icefields also require authorization.
Insurance requirements apply to Icefield Range expeditions.
Cross-border expeditions may also need advance clearance from the appropriate Canadian and U.S. border authorities.
Anyone planning a climb should consult both Parks Canada and the National Park Service well before departure because regulations and administrative requirements can change.
πΏ Flora and Fauna
Mount Saint Elias itself rises far above the elevation where most plants and animals can survive.
Its summit environment consists largely of snow, ice, exposed rock, wind, and severe cold.
Descending toward Icy Bay and the surrounding protected lands, however, reveals a remarkable ecological transition.
π² Plant Life
The coastal portion of Wrangell-St. Elias National Park and Preserve receives substantial Pacific moisture and supports lush vegetation at low elevations.
Plant communities can include:
- Sitka spruce
- Willow
- Alder
- Blueberry
- Crowberry
- Sedges
- Grasses
- Mosses
- Lichens
Farther inland, boreal species such as black spruce and white spruce become more important.
As elevation increases, trees give way to shrubs and alpine tundra.
Eventually, even hardy alpine plants disappear and the landscape becomes dominated by glacier ice and bare rock.
Wrangell-St. Elias as a whole contains hundreds of vascular plant species because of its enormous size and mixture of coastal, transitional, and interior climates.

π» Wildlife
Wildlife is concentrated well below the summit but thrives throughout the broader protected landscape.
Species found in Wrangell-St. Elias include:
- Dall sheep
- Mountain goats
- Caribou
- Moose
- Brown bears
- Black bears
- Wolves
- Wolverines
- Lynx
- Foxes
- Arctic ground squirrels
- Pikas
- Porcupines
The coastal environment around Icy Bay supports additional wildlife.
Harbor seals, sea otters, sea lions, porpoises, and whales may occur in the surrounding marine waters.
Migratory birds also pass through the Yakutat coastal region in large numbers.
The transition from marine ecosystems to an 18,000-foot alpine summit within such a short distance is one of the remarkable ecological characteristics of the Saint Elias landscape.
ποΈ Two Great National Parks
Mount Saint Elias belongs to two extraordinary protected areas.
Wrangell-St. Elias National Park and Preserve
The American side lies within Wrangell-St. Elias National Park and Preserve, the largest unit in the U.S. National Park System.
The park protects more than 13 million acres of mountains, volcanoes, glaciers, rivers, forests, tundra, coastal ecosystems, wildlife habitat, historic sites, and Indigenous cultural landscapes.
Kluane National Park and Reserve
The Canadian side lies within Kluane National Park and Reserve in Yukon.
Kluane contains Canada’s highest mountain, Mount Logan, along with enormous icefields and many of Canada’s highest summits.
Together with Glacier Bay National Park and Preserve and Tatshenshini-Alsek Provincial Park, these parks belong to the Kluane/Wrangell-St. Elias/Glacier Bay/Tatshenshini-Alsek UNESCO World Heritage Site.
It is one of the greatest protected mountain-and-glacier landscapes on Earth.
π Can You See Mount Saint Elias Without Climbing?
Yes, although weather frequently determines whether visitors actually get a clear view.
The Yakutat and Icy Bay region provides opportunities to see portions of the Saint Elias Mountains.
Yakutat itself is accessible primarily by air or sea rather than road.
Flightseeing can provide especially dramatic views of glaciers, icefields, and mountains when weather permits.
The mountain can also sometimes be seen from offshore.
Because Pacific storms frequently blanket the summit in cloud, seeing Mount Saint Elias completely unobscured can be an event in itself.
β°οΈ Nearby Mountains
Mount Saint Elias stands among some of the greatest peaks in North America.
Mount Logan
At 19,550 feet, Mount Logan is Canada’s highest mountain and the second-highest summit in North America.
It lies roughly 26 miles northeast of Saint Elias and is Saint Elias’s parent peak.
Mount Vancouver
Mount Vancouver is another major border summit in the Saint Elias Mountains.
Its massif rises between Alaska and Yukon northwest of Mount Saint Elias.
Mount Fairweather
Farther southeast, Mount Fairweather rises along the AlaskaβBritish Columbia border and reaches 15,324 feet.
Its dramatic position near the Gulf of Alaska makes it another outstanding example of the enormous relief characteristic of the coastal Saint Elias Mountains.
These peaks form part of an almost continuous world of icefields, glaciers, ridges, and high summits stretching across southeastern Alaska, Yukon, and northwestern British Columbia.
β Why Mount Saint Elias Is Special
Mount Saint Elias combines qualities rarely found in a single mountain.
It rises more than 18,000 feet, yet stands extraordinarily close to the sea.
It forms an international boundary, belongs to two national parks, possesses more than 11,000 feet of prominence, and sits at the heart of one of the most active mountain-building regions in North America.
Its glaciers connect the summit to the coastal landscape below.
Its climbing history reaches back to the heroic era of late-19th-century exploration.
Its Indigenous history reaches much farther back, with Was’eitushaa holding enduring cultural and spiritual importance for the Yakutat Tlingit.
Mount Saint Elias is therefore much more than the second-highest mountain in two countries.
It is a place where ocean, glacier, tectonics, wilderness, culture, and extreme mountaineering all converge in one extraordinary landscape.
π Related Articles
- Mount Logan
- Mount Vancouver
- Mount Fairweather
- Mount Wrangell
- Mount Sanford (Alaska)
- Mount Blackburn
- Mount Drum
π Sources
- National Park Service β Mount St. Elias: Yakutat Tlingit Ethnographic Study
- National Park Service β First Ascent of Mount Saint Elias
- National Park Service β Who Were Wrangell and St. Elias?
- National Park Service β Geology of Wrangell-St. Elias National Park and Preserve
- National Park Service β Mountaineering in Wrangell-St. Elias
- National Park Service β Yakutat and Coastal Area
- National Park Service β Plants of Wrangell-St. Elias
- National Park Service β Mammals of Wrangell-St. Elias
- Parks Canada β Kluane National Park and Reserve Mountaineering Permits
- U.S. Geological Survey β Geology of the Yakutat Terrane and Saint Elias Region
- American Alpine Club β Mount Saint Elias First Winter Ascent
- Peakbagger β Mount Saint Elias
