Grosses Wannenhorn

🏔️ Overview
Grosses Wannenhorn is a heavily glaciated mountain rising to 3,906 meters (12,815 feet) in the Bernese Alps of southern Switzerland. Located entirely within the canton of Valais, the mountain stands between two of the Alps’ most important ice streams: the Great Aletsch Glacier to the west and the Fiescher Glacier to the east.
The mountain belongs to the Walliser Fiescherhörner, a line of peaks that also includes Fiescher Gabelhorn, Schönbühlhorn, Kleines Wannenhorn, and the Wannenzwillinge. Grosses Wannenhorn is the highest summit in this group.
Although it falls just short of the symbolic 4,000-meter mark, Grosses Wannenhorn has considerable topographic independence. Its broad glaciated slopes, substantial prominence, and position overlooking the Aletsch Glacier make it one of the more distinctive high mountains in this part of the Swiss Alps.
Swiss sources may also refer to the mountain as Gross Wannenhorn. Because the German letter “ß” is not used in Swiss Standard German, the name is written with “ss” rather than Großes Wannenhorn.
⚡ Fast Facts
| Fact | Details |
|---|---|
| Continent | Europe |
| Country | Switzerland |
| State/Province | Canton of Valais |
| County/Region | Goms District |
| Mountain Range | Bernese Alps; Walliser Fiescherhörner |
| Parent Peak | Finsteraarhorn |
| Elevation | 3,906 meters / 12,815 feet |
| Prominence | Approximately 632 meters / 2,074 feet |
| Isolation | Approximately 4.3 kilometers / 2.7 miles |
| Nearest Higher Neighbor (NHN) | Gross Grünhorn |
| Coordinates | 46.4938° N, 8.0976° E |
| First Ascent | 1864, by Gottlieb Studer and party |
| Normal Base | Finsteraarhornhütte SAC |
| Notable Feature | Separates the Aletsch and Fiescher glacier systems |
📍 Location
Grosses Wannenhorn is located in the Goms region of Valais, northwest of the village of Fiesch and west of the upper Fiescher Glacier. The mountain lies within the Swiss Alps Jungfrau-Aletsch World Heritage Site, an internationally protected landscape containing many of the highest mountains and largest glaciers in the Alps.
Its position is especially notable because the mountain forms part of the divide between two major glacial basins. The Aletsch Glacier system stretches along its western side, while the Fiescher Glacier descends to the east.
The nearest valley communities include Fiesch, Fieschertal, Bellwald, and the Aletsch Plateau villages. However, the summit itself is surrounded by glaciers and remote high-alpine terrain. Reaching it requires a lengthy approach, usually involving an overnight stay at a mountain hut.
The mountain’s approximate coordinates are 46.4938° north and 8.0976° east.
📏 Elevation & Prominence
Grosses Wannenhorn has a commonly accepted elevation of 3,906 meters, equivalent to approximately 12,815 feet. More precise databases may record the summit at about 3,905.5 meters, but Swiss maps and most mountaineering references round the figure to 3,906 meters.
Its topographic prominence is approximately 632 meters, although some sources calculate a slightly higher figure of around 636 meters. These small differences generally result from the map edition, summit measurement, and key-col elevation used in the calculation.
The mountain’s key col lies near the Grünhornlücke, a high glacial pass connecting the Fiescher Glacier basin with the Aletsch Glacier system. Grosses Wannenhorn’s substantial prominence gives it a much stronger individual profile than many of the nearby subsidiary summits.
Its nearest higher terrain lies roughly 4.3 kilometers to the north-northwest on Gross Grünhorn, which rises to just over 4,040 meters. The mountain’s broader topographic parent is the 4,274-meter Finsteraarhorn, the highest mountain in the Bernese Alps.
For more information about these measurements, see What Is Mountain Prominence? and Mountain Elevation vs. Prominence.

🪨 Geology
Grosses Wannenhorn stands within one of the most geologically important landscapes in the European Alps. The wider Jungfrau-Aletsch region contains ancient crystalline rocks, some of which formed hundreds of millions of years ago before being uplifted during the creation of the Alps.
The modern mountain landscape developed as the African and European tectonic plates converged. Compression, folding, faulting, and uplift intensified between approximately 20 and 40 million years ago, gradually raising the high Alpine chain.
Glaciers later reshaped the mountains. Moving ice excavated valleys, steepened ridges, widened basins, and carried enormous quantities of broken rock downstream. Repeated glacial advances helped produce the dramatic contrast between Grosses Wannenhorn’s different faces:
- The eastern side is covered by broad snowfields and glaciers.
- The western side is considerably steeper and is interrupted by rock walls and hanging ice fields.
- The southern ridge continues toward Kleines Wannenhorn and the Wannenzwillinge.
Freeze-thaw weathering continues to fracture exposed rock. Water enters cracks during warmer periods, freezes when temperatures fall, and gradually expands the fractures. This process contributes to rockfall and makes conditions on high Alpine routes change over time.
Learn more about the forces responsible for landscapes like Grosses Wannenhorn in How Are Mountains Formed?.
🌿 Flora & Fauna
The summit and upper slopes of Grosses Wannenhorn lie within the nival zone, where permanent snow, exposed rock, and glacial ice dominate the landscape. Vegetation is extremely limited at these elevations.
Lichens, mosses, algae, and a small number of cold-tolerant plants may survive on isolated patches of stable rock. Lower down, newly exposed glacier forefields provide important examples of ecological succession. Pioneer plants gradually colonize bare sediment after the ice retreats, eventually helping to create conditions suitable for more complex plant communities.
The lower Aletsch region contains a far greater variety of vegetation. Swiss stone pine, European larch, Norway spruce, alpine rose, and numerous meadow flowers grow in the forests and pastures below the glaciated high mountains.
Animals found within the broader Aletsch landscape include:
- Alpine chamois
- Alpine marmots
- Red deer
- Alpine ibex
- Mountain hares
- Golden eagles
- Black grouse
- Spotted nutcrackers
Most large mammals remain well below the summit, where food and shelter are available. Birds may occasionally be seen flying over the glaciers or searching for food along rocky ridges.

🥾 Hiking & Climbing Routes
Grosses Wannenhorn is not a conventional hiking mountain. Every summit route crosses glaciers or technical alpine terrain, requiring experience with crampons, an ice axe, roped glacier travel, crevasse rescue, and rapidly changing mountain weather.
Northeast Flank and East Ridge
The usual ascent begins at the Finsteraarhornhütte SAC, situated at approximately 3,048 meters above the Fiescher Glacier.
From the hut, climbers descend toward the glacier before approaching the broad northeastern side of Grosses Wannenhorn. The route crosses heavily crevassed terrain and climbs the glaciated northeast flank toward the upper east ridge.
Although the technical climbing is relatively moderate under favorable conditions, crevasses, navigation difficulties, ice, and poor visibility can make the route serious. Conditions may change substantially during the season.
Ski-Touring Route from Finsteraarhornhütte
Grosses Wannenhorn is also a recognized spring ski-touring summit. The Swiss Alpine Club grades the ski ascent from the Finsteraarhornhütte approximately PD+.
The route involves about:
- 1,280 meters of ascent
- Three and a half to four hours of climbing
- Predominantly north- and northeast-facing terrain
Large crevasses are among the principal hazards. Skiers normally descend along the ascent route unless undertaking a longer and more difficult descent toward Fieschertal.
Schönbühlhorn–Wannenhorn Traverse
A much more demanding possibility follows the ridge from Schönbühlhorn toward Grosses Wannenhorn. This traverse involves exposed rock, snow, ice, and complex route-finding.
The ridge is significantly more difficult and committing than the normal glacial route. It should only be attempted by experienced alpinists in stable conditions.
Southeast Ridge and Other Routes
The southeast ridge provides another technical route to the summit. Other historical lines have been climbed on the north face, northwest ridge, southwest flank, and adjoining ridges, but these routes are less frequently attempted and may be highly dependent on snow, ice, and rock conditions.
Grosses Wannenhorn has two closely connected summit points: a rocky northern summit and a flatter southern summit joined by a short ridge.
🏔️ Field Guide Tip: Even the normal route crosses a crevassed glacier. Check current conditions with the Finsteraarhornhütte or a qualified local mountain guide, and never rely solely on an older route description or GPS track.
🌤️ Best Time to Visit
The best season depends on the intended activity.
Summer Mountaineering
The main mountaineering season generally runs from late June through September. Early summer may provide better snow bridges over crevasses, while later summer can expose larger crevasses and unstable rock.
Warm summers may cause route conditions to deteriorate earlier than expected. An ascent that was straightforward one year may become more complicated the next because of glacier retreat or reduced snow cover.
Spring Ski Touring
Ski ascents are most often attempted during the late-winter and spring touring season, commonly from March through May. Climbers usually begin very early to take advantage of firm snow and reduce exposure to warming slopes.
Regardless of season, the safest period is determined by current weather, avalanche conditions, glacier coverage, and reports from local guides and hut staff.

🧭 Nearby Mountains & Attractions
Grosses Wannenhorn is surrounded by some of the most impressive peaks and glaciers in Switzerland.
Gross Grünhorn
The Gross Grünhorn rises north-northwest of Grosses Wannenhorn and is its nearest higher neighbor. At more than 4,040 meters, it is one of the major summits overlooking the upper Aletsch Glacier.
Finsteraarhorn
The Finsteraarhorn is the highest mountain in the Bernese Alps. Its sharply defined summit rises east of the upper Fiescher Glacier and dominates much of the surrounding landscape.
Grosses Fiescherhorn
The Grosses Fiescherhorn is a 4,000-meter peak north of Grosses Wannenhorn. It forms part of the high glaciated chain between the Fiescher Glacier and the Jungfrau region.
Hinteres Fiescherhorn
The Hinteres Fiescherhorn stands close to the Grosses Fiescherhorn. It is frequently climbed from the Finsteraarhornhütte or combined with neighboring summits.
Fiescher Gabelhorn
The Fiescher Gabelhorn is part of the same Walliser Fiescherhörner group as Grosses Wannenhorn. Schönbühlhorn lies between the two principal summits.
Aletschhorn
Across the Aletsch Glacier stands the Aletschhorn, the second-highest mountain in the Bernese Alps and one of the most prominent peaks in Switzerland.
Great Aletsch Glacier
The Great Aletsch Glacier flows west of Grosses Wannenhorn. It is the largest glacier in the Alps and the central natural feature of the Jungfrau-Aletsch World Heritage Site.
Fiescher Glacier
The Fiescher Glacier lies directly east of the mountain. It provides access to the Finsteraarhornhütte and serves as part of several major mountaineering and ski-touring routes.
💡 Fun Facts
- Grosses Wannenhorn is the highest summit of the Walliser Fiescherhörner.
- It is approximately 94 meters short of becoming a 4,000-meter Alpine peak.
- The mountain has two summit points connected by a short ridge.
- Its northern summit is rocky, while the southern summit is broader and flatter.
- The mountain separates the Aletsch and Fiescher glacier systems.
- Its first recorded ascent was completed in 1864 by Gottlieb Studer and his companions.
- Grosses Wannenhorn has more than 600 meters of prominence, making it considerably more independent than many nearby Alpine summits.
- The summit provides an exceptional view over the Great Aletsch Glacier and many of the Bernese Alps’ 4,000-meter mountains.
❓ Frequently Asked Questions

How high is Grosses Wannenhorn?
Grosses Wannenhorn rises to approximately 3,906 meters, or 12,815 feet, above sea level.
Where is Grosses Wannenhorn?
The mountain is in the canton of Valais, Switzerland. It stands between the Great Aletsch Glacier and the Fiescher Glacier in the Bernese Alps.
Is Grosses Wannenhorn a 4,000-meter peak?
No. Its summit is about 94 meters below 4,000 meters.
Can Grosses Wannenhorn be climbed by hikers?
No marked hiking trail reaches the summit. The normal route involves crevassed glaciers and requires mountaineering equipment, glacier-travel skills, and appropriate experience.
What is the normal route?
The most commonly used route begins at the Finsteraarhornhütte and climbs the mountain’s northeastern glaciated slopes before reaching the east ridge and summit area.
What is the nearest higher mountain?
The nearest higher neighbor is Gross Grünhorn, located roughly 4.3 kilometers to the north-northwest.
What is the best time to climb Grosses Wannenhorn?
Summer ascents are generally attempted between late June and September. Ski tours are more common during late winter and spring. Actual suitability depends on current glacier, avalanche, snow, and weather conditions.
Who made the first ascent?
The first recorded ascent was completed in 1864 by Swiss mountaineer Gottlieb Studer and his party.
🔗 Related Articles
- The Alps
- Finsteraarhorn
- Grünhorn
- Grosses Fiescherhorn
- Hinteres Fiescherhorn
- Fiescher Gabelhorn
- Aletschhorn
- Klein Grünhorn
- Trugberg
Related Hiking and Safety Guides
- The Ten Essentials for Hiking
- What to Do If You Get Lost Hiking
- What Is Mountain Prominence?
- Mountain Elevation vs. Prominence
- How Are Mountains Formed?
📚 Sources
- Peakbagger – Switzerland Peaks with 600 Meters of Prominence
- Swiss Alpine Club – Grosses Wannenhorn Alpinism
- Swiss Alpine Club – Grosses Wannenhorn Ski Touring
- PeakVisor – Grosses Wannenhorn
- UNESCO World Heritage Centre – Swiss Alps Jungfrau-Aletsch
- Pro Natura Aletsch – Aletsch Forest Nature Reserve
- Grosses Wannenhorn – Wikipedia