Melungtse: The Highest Mountain of the Rolwaling Himal

Melungtse (Jobo Garu, 乔格茹峰, Qiáogérú Fēng, Menlungtse)

🏔️ Overview

Melungtse is a remote and striking Himalayan mountain rising to 7,181 meters (23,560 feet) in the Tibet Autonomous Region of China. It is the highest summit of the Rolwaling Himal, a rugged section of the Himalayas extending along the borderlands of Nepal and Tibet.

Although Melungtse is higher than the nearby and better-known Gauri Sankar, it receives far less attention. Gauri Sankar is prominently visible from populated areas of Nepal, while Melungtse stands farther north, partly concealed behind the main Rolwaling ridges. Its isolated position, restricted access, and formidable climbing terrain have helped keep it one of the more obscure mountains above 7,000 meters.

The mountain has a long, complex summit ridge containing two principal high points. The eastern summit is the 7,181-meter main summit, while the western summit—usually called Melungtse II—reaches approximately 7,023 meters (23,041 feet). A ridge roughly two kilometers long separates the two summits, but traversing it involves steep, exposed, and heavily corniced terrain.

Melungtse is not simply a high snow peak. It is surrounded by immense walls of rock and ice, hanging glaciers, sharp ridges, and avalanche-prone slopes. Its faces rise abruptly from the surrounding valleys, giving the mountain a greater sense of scale and seriousness than its elevation alone might suggest.

The main summit was first reached on October 23, 1992, when Slovenian climbers Marko Prezelj and Andrej Štremfelj completed an exceptionally difficult alpine-style ascent of the southeast face. Their climb remains one of the defining achievements associated with the mountain.

⚡ Fast Facts

Fact	Details
Continent	Asia
Country	China
State/Province	Tibet Autonomous Region
County/Region	Tingri County, Shigatse
Mountain Range	Rolwaling Himal, Himalayas
Parent Peak	Mount Everest, following its broader topographic lineage
Elevation	7,181 meters / 23,560 feet
Prominence	Approximately 1,570 meters / 5,151 feet
Isolation	Approximately 21.2 kilometers / 13.2 miles
Nearest Higher Neighbor	Cho Aui, also known as Nangpai Gosum I
Nearest Higher Neighbor Elevation	Approximately 7,350 meters / 24,114 feet
Coordinates	Approximately 27.9716° N, 86.4309° E
Secondary Summit	Melungtse II, approximately 7,023 meters / 23,041 feet
First Ascent of Main Summit	October 23, 1992
First Ascenders	Marko Prezelj and Andrej Štremfelj
Alternate Spelling	Menlungtse
Mountain Type	Glaciated high Himalayan peak
Topographic Classification	Ultra-prominent mountain

Prominence figures differ slightly among topographic databases. Some sources list approximately 1,551 meters, while others calculate about 1,570 meters. Both values place Melungtse above the 1,500-meter threshold required for classification as an ultra-prominent summit. Its nearest higher terrain is associated with Cho Aui or Nangpai Gosum I, approximately 21.2 kilometers to the east-northeast.

📍 Location

Melungtse stands in Tingri County, within the Shigatse administrative region of the Tibet Autonomous Region. It lies just north of the international boundary between China and Nepal rather than directly on the border itself.

This distinction is important because Melungtse is sometimes loosely described as a Nepalese or Nepal–Tibet border mountain. The Rolwaling Himal spans both countries, and many views of Melungtse are obtained from Nepal, but the main summit and Melungtse II are located on the Tibetan side.

The mountain rises from a western spur extending away from the principal north–south ridge of the Rolwaling Himal. The Menlung Chu valley separates the Melungtse massif from Gauri Sankar to the southwest. Gauri Sankar reaches 7,134 meters and stands much closer to the border, making it considerably more prominent when seen from Nepal.

Melungtse is approximately 40 kilometers west of Mount Everest. Farther east, the Rolwaling mountains approach the Nangpa La region, where the Rolwaling Himal meets the better-known Mahalangur Himal containing Cho Oyu, Everest, Lhotse, and Makalu.

Despite this proximity to the Everest region, Melungtse belongs to a very different mountaineering environment. Commercial climbing infrastructure is limited, approaches are complicated by political boundaries, and there is no heavily traveled standard route comparable to those found on Everest or Cho Oyu.

Relationship to the Rolwaling Valley

The Rolwaling Valley lies south of the main Himalayan divide in Nepal’s Dolakha District. It is an isolated high valley surrounded by steep ridges, glaciers, and numerous summits above 6,000 meters.

Communities such as Beding and Na are situated deep within the Nepalese side of the valley. The region is known for challenging trekking routes, traditional Sherpa settlements, and access to high-altitude destinations such as Tsho Rolpa and the Tashi Lapcha crossing.

Melungtse rises beyond the ridges north of the valley. Depending on weather, season, and viewpoint, parts of the massif may be seen from high locations in Nepal. Its position behind the more immediate border peaks, however, means that it is not always easily distinguished.

This relative concealment partly explains why Gauri Sankar became the symbolic mountain of the Rolwaling region even though Melungtse is 47 meters higher. Gauri Sankar presents an unmistakable twin-summited profile from Nepal, whereas Melungtse is more distant and frequently hidden by intervening ridges.

🏔️ Field Guide Tip: Melungtse should not be confused with an ordinary trekking peak in Nepal’s Rolwaling Valley. Trekkers may obtain distant views of the mountain from the Nepalese side, but reaching or climbing Melungtse involves separate access to its Tibetan approaches and the organization of a major technical expedition.

📏 Elevation and Prominence

Melungtse’s accepted elevation is 7,181 meters, equivalent to 23,560 feet. This makes it the highest mountain in the Rolwaling Himal and one of the substantial 7,000-meter summits of the greater Himalayan system.

Its elevation places it slightly above Gauri Sankar:

Mountain	Elevation
Melungtse	7,181 m / 23,560 ft
Gauri Sankar	7,134 m / 23,406 ft
Melungtse II	7,023 m / 23,041 ft

The 47-meter difference between Melungtse and Gauri Sankar is small when compared with the immense scale of both mountains. Visibility rather than elevation has therefore shaped their relative fame. Gauri Sankar dominates several views from Nepal, while the higher Melungtse remains comparatively hidden.

Topographic Prominence

Topographic prominence measures how far a mountain rises above the lowest saddle connecting it to higher terrain. It provides a way of evaluating the mountain’s independence rather than simply its height above sea level.

Melungtse has a prominence of approximately 1,570 meters, although some calculations give 1,551 meters. Under either measurement, the mountain qualifies as an ultra-prominent peak, meaning that it rises at least 1,500 meters above its key saddle.

This substantial prominence demonstrates that Melungtse is not merely a minor point on a larger Himalayan ridge. It forms the commanding high point of its own massif and dominates a large section of the Rolwaling Himal.

Isolation and Nearest Higher Neighbor

Melungtse has a topographic isolation of approximately 21.2 kilometers. This is the distance from its summit to the nearest location reaching a greater elevation.

The nearest higher neighbor is generally identified as Cho Aui, a name associated with Nangpai Gosum I, which rises to around 7,350 meters east-northeast of Melungtse. Naming conventions in the Nangpai Gosum group have changed over time, so different topographic and mountaineering sources may use Cho Aui, Nangpai Gosum I, Jasemba, or Pasang Lhamu Chuli for related summits in the massif.

🪨 Geology

Detailed geological descriptions written specifically about Melungtse are limited. However, regional mapping of the Rolwaling and upper Tama Kosi areas provides a useful picture of the mountain’s broader geological setting.

The Rolwaling Himal forms part of the high-grade crystalline core of the Himalayan mountain system. The region contains metamorphic rocks associated with the Greater Himalayan Sequence, including:

• Paragneiss formed from metamorphosed sedimentary rocks
• Orthogneiss derived from older igneous rocks
• Mica-rich schists
• Migmatites altered by intense heat and partial melting
• Granitic and leucogranitic intrusions

These rocks were buried, heated, compressed, deformed, and eventually uplifted during the ongoing collision between the Indian and Eurasian tectonic plates. Geological research in the adjacent Rolwaling region records increasing metamorphic intensity toward the higher structural levels of the range, along with widespread folding, shearing, and deformation.

Formation of the Rolwaling Himal

The Himalayas began forming tens of millions of years ago as the Indian continental plate moved northward and collided with Eurasia. Because both plates consist largely of buoyant continental crust, neither could easily descend into the mantle. Instead, the crust shortened, folded, fractured, and thickened.

Large packages of rock were pushed southward along major fault systems. At the same time, deeply buried rocks were subjected to high pressures and temperatures before being carried upward through uplift and erosion.

Melungtse is part of this uplifted crystalline terrain. Its present summit represents only the surviving upper portion of a much larger geological structure continually modified by frost, ice, gravity, and glacial erosion.

Glacial Sculpting

The sharp form seen today developed through repeated periods of glaciation. Moving ice excavated the valleys around the massif, while freeze-thaw weathering loosened blocks from exposed ridges and faces.

Snow and ice accumulated in shaded basins, forming glaciers that flowed away from the mountain. These glaciers deepened valleys and steepened surrounding walls, leaving Melungtse with its dramatic relief.

Modern photographs show a mountain dominated by:

• Steep snow and ice faces
• Narrow, corniced ridges
• Hanging glaciers
• Deep couloirs
• Serac formations
• Avalanche channels
• Exposed sections of dark rock

These features make the mountain especially hazardous. Cornices can collapse without warning, seracs may break from hanging glaciers, and snow deposited on the steep faces can produce large avalanches.

The Two Summits of Melungtse

Melungtse’s architecture is unusual enough that its two summits are often treated as separate climbing objectives.

Main Summit

The main summit stands at the northeastern end of the high ridge and reaches 7,181 meters. It is generally called Melungtse, Melungtse I, or the east summit.

This was the objective reached by Marko Prezelj and Andrej Štremfelj in 1992. The summit is defended by steep faces on several sides and offers no straightforward walking route.

Melungtse II

Melungtse II forms the western high point of the massif and reaches approximately 7,023 meters. It was climbed before the main summit, when British mountaineers Andy Fanshawe and Alan Hinkes reached it during an expedition led by Chris Bonington.

Although sometimes referred to as a subsidiary summit, Melungtse II is itself higher than many famous independent Himalayan mountains. The long connecting ridge between it and the main summit is highly technical, explaining why reaching Melungtse II did not provide a simple continuation to the higher top.

Together, the two summits create Melungtse’s distinctive elongated profile: a broad, heavily glaciated mountain crowned by multiple high points rather than a single isolated pyramid.

🌿 Flora and Fauna

Melungtse’s upper slopes are too high, cold, and heavily glaciated to support substantial plant or animal life. Above approximately 5,500 meters, the landscape is dominated by exposed rock, permanent snow, glacier ice, and wind-scoured ridges. Nevertheless, the valleys surrounding the mountain contain unexpectedly varied habitats.

The Tibetan Plateau north of the Himalayas is generally dry, but the Rongshar and Menlung valleys lie south of the main watershed and receive greater moisture from weather systems moving north from Nepal. As a result, the lower approaches to Melungtse are considerably greener than the open plateau around Tingri.

Historical expedition accounts describe narrow gorges containing dense vegetation, high pastures, and forests extending into the Menlung Valley. The approach passes through several ecological zones, ranging from wooded valleys to alpine meadows and finally to glacial terrain.

Forests of the Menlung Valley

The lower Menlung Chu cuts through forests containing:

• Rhododendron
• Bamboo
• Juniper
• Fir and other conifers
• Alpine shrubs
• Grasses and seasonal wildflowers

Rhododendrons can form dense stands on sheltered slopes, producing vivid flowers during the spring. Bamboo grows in wetter sections of the valley, while conifers occupy cooler hillsides and ravines.

Juniper becomes more common near the upper limit of substantial vegetation. At around 4,000 meters, historic expedition base camps were established on grassy shelves surrounded by juniper-covered slopes and rhododendron forest.

Above the forest line, trees give way to alpine grasslands used historically by yak herders. These meadows provide some of the few relatively level camping areas in a landscape otherwise dominated by steep slopes, moraines, and glaciers.

Alpine Vegetation

The short Himalayan summer allows hardy alpine plants to grow in sheltered areas. Mosses, lichens, cushion plants, sedges, and low flowering herbs may appear between rocks where soil and moisture accumulate.

Conditions become increasingly severe with elevation. Plants must withstand:

• Intense ultraviolet radiation
• Strong winds
• Large daily temperature changes
• Frozen ground
• A very short growing season
• Snow cover lasting much of the year

Near Melungtse’s glaciers, vegetation is generally limited to patches of grass and low plants growing on stable moraine surfaces. Freshly exposed glacial debris may remain almost completely barren.

Wildlife of the Region

Systematic wildlife surveys specifically focused on Melungtse are limited. However, the broader Rolwaling–Rongshar landscape provides habitat for several high-altitude Himalayan species.

Potential mammals of the surrounding valleys and ridges include:

• Snow leopards
• Himalayan blue sheep
• Himalayan tahr
• Musk deer
• Himalayan marmots
• Pikas
• Red foxes
• Weasels and other small carnivores

Snow leopards are particularly significant because their presence near Melungtse is not merely theoretical. During the 1990 American expedition, climber John Roskelley reportedly came within a few feet of a snow leopard while carrying supplies along a moraine.

Large birds may also use the valleys and high ridges. Himalayan griffon vultures, lammergeiers, golden eagles, ravens, and choughs are capable of traveling through high mountain environments, although they are more likely to be seen above valleys and cliffs than on the mountain’s glaciated summit ridge.

🏔️ Field Guide Tip: Wildlife sightings are uncommon in open glacial terrain, but tracks may be easier to notice on snow or soft moraine surfaces. Animals in remote Himalayan valleys should be observed from a distance and never approached or fed.

🥾 Hiking and Climbing Routes

Melungtse is not a trekking summit and has no ordinary hiking route to its highest point. Every known line involves serious high-altitude mountaineering on steep rock, ice, snow, or mixed terrain.

Even reaching the base of the mountain has historically required a long and complicated expedition. Teams have approached through Tibet using the Rongshar Valley and the Menlung Chu, transporting equipment with yaks before establishing base camps at roughly 4,000 to 4,800 meters.

The absence of a straightforward route is one of Melungtse’s defining characteristics. Each side of the mountain is guarded by a combination of steep walls, unstable rock, hanging glaciers, corniced ridges, and avalanche-prone snowfields.

Is There a Normal Route?

Melungtse does not have a normal route comparable to the standard paths on frequently climbed Himalayan peaks.

The southeast face, used for the first ascent of the main summit, is the mountain’s only confirmed route to the 7,181-meter summit. However, it should not be considered an established or routinely repeatable route. It remains an extremely serious alpine climb exposed to objective hazards.

Melungtse II has been reached by the west ridge and west face system, but the route includes difficult mixed climbing, loose rock, steep ice, bergschrunds, and a dangerous upper headwall.

Early Exploration

The Menlung Valley was reached by European explorers during the first half of the 20th century, but Melungtse remained largely unknown to international mountaineers.

Eric Shipton and Michael Ward visited the valley in 1951 while returning from an Everest reconnaissance expedition. They applied the name Menlungtse to the prominent mountain north of the valley, apparently without knowing that local residents called it Jobo Garu.

The same journey became famous for photographs of unusual tracks found in the snow, later associated with the Himalayan yeti tradition. The tracks contributed to the sense of mystery surrounding the Menlung Valley, although they provide no scientific evidence for an unknown human-like creature.

The 1987 South-Southwest Buttress Attempt

Chris Bonington led a British-Norwegian expedition to Melungtse in 1987. The team approached the mountain from Tibet and established its base in the Menlung Valley.

After examining the northern side, the climbers concluded that Melungtse’s north and northwest faces were excessively dangerous. Sheer rock walls and hanging seracs guarded much of the terrain.

They therefore turned their attention to the southern side and selected a south-southwest buttress. The lower route involved steep slabs and shattered granite. Approximately 600 meters of rope were fixed before the climbers began an alpine-style summit attempt.

Higher on the buttress, they encountered difficult rock climbing followed by a snow section. Severe storms repeatedly struck the mountain, destroying a tent and forcing the team to retreat. Two additional attempts were also stopped by bad weather.

First Ascent of Melungtse II

Bonington returned in the spring of 1988 with another international expedition. The original goal remained the main summit, but the east ridge appeared extremely long, steep, and heavily corniced.

The team instead investigated the west ridge. After establishing camps and fixing sections of the lower route, Andy Fanshawe and Alan Hinkes made a lightweight summit attempt.

They climbed toward an upper headwall containing loose rock, icy runnels, and mixed terrain. The final obstacle was a difficult overhanging chimney followed by slabs covered with unstable powder snow.

Fanshawe and Hinkes reached the 7,023-meter west summit, now known as Melungtse II, late on May 23, 1988. They had been climbing for approximately 13½ hours and chose not to attempt the long traverse toward the main summit.

The detailed expedition accounts place this ascent in 1988, although some later summaries have incorrectly assigned it to 1987.

The 1990 Southeast Ridge Attempt

An American team consisting of Greg Child, Jim Wickwire, Jeff Duenwald, and John Roskelley attempted the main summit in 1990.

They established an advanced camp beneath the southeast ridge and fixed ropes over steep ice. Roskelley and Child then began an alpine-style push, climbing snow and ice angled at approximately 55 to 60 degrees.

After three nights on the ridge, they reached about 6,460 meters, where the route became a narrow, heavily corniced crest. The cornices were too fragile to cross safely, and the team retreated.

Their experience showed that even a ridge appearing comparatively logical from below could become impassable because of unstable snow formations.

First Ascent of Melungtse

The main summit remained unclimbed until a small Slovenian expedition arrived in autumn 1992.

Marko Prezelj and Andrej Štremfelj, accompanied at base camp by expedition doctor Žarko Guzej, selected a line on the mountain’s immense southeast face. Their route followed terrain to the left of the line attempted by the Americans two years earlier.

The Southeast Face

The face rises approximately 2,000 meters from its base to the summit area. Although not every section required extreme technical climbing, the route was dangerously exposed to falling stones, ice, and avalanches.

Prezelj and Štremfelj established an advanced base at approximately 5,150 meters. Their initial attempt began on October 18, but deteriorating weather and avalanche conditions forced them to descend from around 6,400 meters.

They returned for a second attempt on October 22. Falling rock and ice forced them to shelter in an ice cave at approximately 6,150 meters after only a few hours of climbing.

The following morning, they continued up ice slopes reaching roughly 55 degrees. Moving quickly in alpine style, they gained the upper plateau and continued toward the summit. They reached Melungtse’s 7,181-meter main summit on October 23, 1992.

The ascent was completed without the large network of fixed camps and ropes commonly associated with traditional Himalayan siege expeditions. Speed reduced the climbers’ time on the face, but it also required them to carry their essential equipment and accept a high level of commitment.

Why the First Ascent Was So Significant

The achievement was notable for several reasons:

• Melungtse was one of the highest unclimbed Himalayan summits at the time.
• The successful route climbed a vast and objectively dangerous face.
• The ascent was completed by a two-person climbing team.
• Prezelj and Štremfelj used a fast alpine-style approach.
• Previous expeditions had been stopped by storms, cornices, poor rock, and dangerous ice formations.

The climb demonstrated that a small, highly experienced team could succeed on terrain where larger expeditions had failed. At the same time, it did not make Melungtse accessible to ordinary climbers. The route’s exposure and commitment remain exceptionally high.

Later North Face Attempts

The enormous north face became the focus of later expeditions.

1999 Attempt

A four-person American-Canadian expedition attempted the north face in 1999. The team selected a snow-and-ice line near the eastern side of the wall.

They reached approximately 5,600 meters before heavy snowfall stopped progress. Increasing avalanche danger made continuing unjustifiable, and the climbers abandoned the route.

The team later climbed a nearby 6,262-meter summit, which they named Milarepa after the Tibetan Buddhist teacher traditionally associated with the region.

2005 Attempt

Another expedition returned in 2005 and examined a different line on the western portion of the north face.

The climbers crossed an initial rock barrier using a narrow strip of water ice before continuing over steep snow, mixed terrain, and ice fields. They climbed for five days and reached a broad shelf at approximately 6,300 meters.

An injury-related medical problem affecting one team member forced the climbers to abandon the attempt. They had overcome much of the lower face but still faced a long ridge and summit traverse.

The expedition’s account illustrates the complexity of Melungtse’s north side: even after climbing 1,500 meters of difficult terrain, a team may remain far from the actual summit.

Principal Routes and Attempts

Route	Objective	Result
South-southwest buttress	Main summit	Attempted in 1987; storms forced retreat
West ridge and west face	Melungtse II	First ascent in 1988
Southeast ridge	Main summit	Attempted in 1990; stopped by unstable cornices
Southeast face	Main summit	First ascent in 1992
Eastern north-face line	Main summit	Attempted in 1999; stopped by snowfall and avalanche danger
Western north-face line	Main summit	Attempted in 2005; abandoned after a medical problem

Major Climbing Hazards

Avalanches

Snowstorms moving north from Nepal can deposit large amounts of snow on Melungtse’s faces. Steep ice fields, gullies, and hanging snow slopes can rapidly become avalanche-prone.

Avalanche danger has ended several attempts and was a major concern during the first ascent.

Serac Collapse

Large blocks and towers of glacial ice overhang several approaches. Seracs can collapse without warning, sending ice across routes hundreds or thousands of meters below.

The mountain’s north face is particularly threatened by hanging glaciers.

Cornices

Wind builds enormous cornices along Melungtse’s ridges. These formations may extend far beyond the supporting rock and can break under a climber’s weight.

The 1990 expedition was stopped by a heavily corniced knife-edge ridge despite having reached high on the mountain.

Rockfall

Melungtse contains sections of fractured and unstable granite. Freeze-thaw cycles loosen blocks, while climbers and melting ice can trigger additional rockfall.

Both the 1987 buttress and the route to Melungtse II contained dangerously loose rock.

Extreme Altitude

At 7,181 meters, the summit lies within the zone where the human body cannot fully acclimatize. Climbers face declining strength, impaired judgment, dehydration, frostbite, and potentially fatal altitude illness.

A rapid alpine-style ascent reduces exposure time but leaves little opportunity for recovery when problems arise.

Isolation

The Menlung Valley is remote, and rescue from the mountain would be extraordinarily difficult. Expeditions must be capable of handling injuries, storms, equipment failures, and emergency descents with limited outside assistance.

🏔️ Field Guide Tip: Melungtse is appropriate only for elite high-altitude alpinists with extensive experience on serious mixed faces. Successfully climbing other 7,000-meter mountains would not, by itself, provide adequate preparation for the mountain’s objective dangers.

🌤️ Best Time to Visit

The most favorable periods for viewing or attempting Melungtse are generally the pre-monsoon spring and post-monsoon autumn seasons.

Spring: April to May

Spring can provide comparatively stable climbing windows before the summer monsoon. Temperatures gradually become less severe, while longer daylight hours allow more time for movement.

However, spring storms remain possible. Several historical expeditions experienced heavy snow, thunderstorms, and strong winds during April and May.

Warming temperatures may also increase rockfall and serac activity later in the day. Climbing teams must carefully judge the balance between excessively cold conditions and daytime melting.

Autumn: September to October

Autumn often offers clearer skies after the monsoon, although new snow and powerful winds can still affect the upper mountain.

The first ascent occurred in late October, showing that an autumn expedition can succeed when conditions align. The season’s colder temperatures may help stabilize some snow and ice, but nights become extremely cold and weather windows can be short.

Summer: June to August

The summer monsoon brings cloud, heavy precipitation, unstable snow, and poor visibility to the Himalayan divide. The Tibetan side may receive less rainfall than Nepal, but Melungtse is close enough to the main range to be strongly affected by moisture moving northward.

Summer is generally unsuitable for a major attempt.

Winter: November to March

Winter brings severe cold, strong winds, drifting snow, and short daylight hours. The mountain’s technical difficulties become even more serious under winter conditions.

A winter expedition would involve an exceptional level of risk and commitment.

Actual access depends on permits, local restrictions, transportation conditions, and authorization from Chinese and Tibetan authorities. These requirements can change, so historical expedition approaches should never be treated as current logistical instructions.

🧭 Nearby Mountains and Attractions

Melungtse occupies an extraordinary position between the remote valleys of Tibet and the high Rolwaling landscapes of Nepal. Several famous Himalayan mountains are comparatively close in a straight line, but deep valleys, glaciers, international borders, and limited roads make travel through the region far more complicated than a map might suggest.

Nearby Mountains

Mountain	Elevation	Relationship to Melungtse
Melungtse II	7,023 m / 23,041 ft	Western summit of the Melungtse massif
Gauri Sankar	7,134 m / 23,406 ft	Lies southwest across the Menlung Chu
Nangpai Gosum I	About 7,350 m / 24,114 ft	Nearest higher mountain, east-northeast of Melungtse
Cho Oyu	8,188 m / 26,864 ft	Major 8,000-meter peak northeast of the Rolwaling Himal
Mount Everest	8,848.86 m / 29,032 ft	Approximately 40 kilometers east of Melungtse

Melungtse II

Melungtse II is the mountain’s 7,023-meter western summit. Although it shares the same massif as the main summit, the two high points are separated by a long ridge approximately two kilometers in length.

Andy Fanshawe and Alan Hinkes completed the first ascent of Melungtse II on May 23, 1988. They reached the western summit after climbing loose rock, icy runnels, an overhanging chimney, and snow-covered slabs.

From the summit, the climbers could see the higher eastern top across the connecting saddle and summit ridge. However, darkness, fatigue, difficult terrain, and the distance to the main summit made continuing impractical.

Melungtse II is sometimes described as a subsidiary summit, but at more than 7,000 meters it remains an enormous mountaineering objective in its own right.

Gauri Sankar

Gauri Sankar rises to 7,134 meters southwest of Melungtse. The Menlung Chu valley separates the two massifs.

Despite being 47 meters lower, Gauri Sankar is far more widely recognized in Nepal. Its dramatic twin summits are visible from parts of the Kathmandu Valley and from several locations in eastern Nepal.

The mountain also has considerable cultural significance. Its name combines Gauri, a name associated with the Hindu goddess Parvati, and Sankar, a name associated with Shiva. The two summits have traditionally been interpreted as representing the divine pair.

Gauri Sankar long played an important role in Nepalese geography and timekeeping. Nepal Standard Time is based on a meridian passing near the mountain, giving the country its distinctive offset of five hours and 45 minutes ahead of Coordinated Universal Time.

The mountain’s greater visibility helps explain why it became the symbolic summit of the Rolwaling region even though Melungtse is slightly higher.

Nangpai Gosum

Nangpai Gosum is a complex group of high summits east-northeast of Melungtse near the Nangpa La region. Its naming history is complicated, and individual summits have been identified under names including Nangpai Gosum, Cho Aui, Jasemba, and Pasang Lhamu Chuli.

The group contains the nearest terrain that rises above Melungtse. This relationship determines Melungtse’s topographic isolation, which is approximately 21.2 kilometers.

Nangpai Gosum stands near the transition between the Rolwaling Himal and the Mahalangur Himal, the Himalayan section containing Cho Oyu, Everest, Lhotse, and Makalu.

Cho Oyu

Cho Oyu rises to 8,188 meters on the Nepal–China border northeast of Melungtse. It is the sixth-highest mountain in the world and the closest 8,000-meter mountain to the Melungtse massif.

The mountain stands near Nangpa La, an important historical crossing between Tibet and Nepal’s Khumbu region. Tibetan traders and Sherpa communities used the pass for generations, although modern border controls now restrict movement.

Cho Oyu is much more frequently climbed than Melungtse. Its standard northwest route is generally considered one of the less technically difficult routes on an 8,000-meter mountain, although it still presents the severe dangers of extreme altitude, cold, crevasses, avalanches, and rapidly changing weather.

The contrast between the two mountains is striking. Cho Oyu attracts organized commercial expeditions, while Melungtse remains a highly technical objective without a regularly repeated route.

Mount Everest

Mount Everest lies approximately 40 kilometers east of Melungtse. From elevated viewpoints, the two mountains form part of the same sweeping Himalayan panorama, although intervening ridges may obscure one or both summits.

Everest belongs to the Mahalangur Himal rather than the Rolwaling Himal. Its enormous elevation and global fame have made the surrounding region one of the busiest high-altitude destinations in the world.

Melungtse exists in a very different setting. It has no commercial base-camp community, permanent climbing infrastructure, established summit traffic, or regularly maintained route. Its remoteness and technical difficulty have preserved a sense of isolation despite its proximity to Earth’s highest mountain.

Rolwaling Valley

The Rolwaling Valley lies on the Nepalese side of the Himalayas south of Melungtse. It is a deep, glacially carved valley containing forests, alpine meadows, traditional settlements, glaciers, and high mountain passes.

Beding is the principal permanent settlement in the upper valley. Farther upstream, the seasonal settlement of Na occupies an open alpine basin surrounded by high mountains.

The valley provides access to views of the broader Rolwaling Himal, although Melungtse itself may remain partly concealed behind intervening ridges. Trekking in Rolwaling does not provide access to Melungtse’s climbing routes, which are on the Tibetan side of the international border.

Compared with the neighboring Everest region, Rolwaling receives relatively few visitors. Its trails can be demanding, facilities are limited, and several routes require experienced guides or technical mountaineering skills.

Tsho Rolpa

Tsho Rolpa is a large glacial lake near the head of Nepal’s Rolwaling Valley. It formed as glaciers retreated and meltwater accumulated behind natural moraine deposits.

The lake has been closely studied because of the danger of a glacial lake outburst flood. Engineering work has lowered its water level and reduced some of the immediate risk, although continued monitoring remains important.

Tsho Rolpa has also become one of the principal trekking destinations in the valley. The route passes through settlements, forests, open pastures, and glacial terrain before reaching the lake beneath the surrounding Himalayan peaks.

Tashi Lapcha Pass

Tashi Lapcha is a difficult high-altitude crossing connecting the Rolwaling Valley with the Khumbu region of Nepal.

The journey is substantially more demanding than an ordinary trekking pass. Snow, ice, crevasses, rockfall, steep slopes, route-finding difficulties, and changing glacier conditions may require ropes, crampons, ice axes, and mountaineering experience.

The pass has historical importance as a connection between two major Sherpa regions. Today, it is undertaken primarily by experienced trekking and climbing groups rather than ordinary hikers.

Menlung and Rongshar Valleys

The traditional northern approach to Melungtse passes through the Rongshar and Menlung valleys in Tibet.

These valleys are unusually green compared with the dry Tibetan Plateau. They contain rhododendron, bamboo, conifer forest, high pastures, steep gorges, and scattered settlements.

Historical expeditions traveled with yak caravans through the region before establishing base camps beneath Melungtse. The journey was a major undertaking in itself, often requiring negotiations for transport animals, changes of caravan crews, and several days of travel beyond the nearest roads.

The area also contains the remains of Chuar Monastery and caves associated in local tradition with the Tibetan Buddhist teacher Milarepa.

🏔️ Field Guide Tip: A trek through Nepal’s Rolwaling Valley and an expedition to Melungtse are entirely different undertakings. The international border, restricted Tibetan access, and the mountain’s northern approaches prevent trekkers from simply continuing from Nepal to Melungtse Base Camp.

💡 Fun Facts

Melungtse Is Higher Than Gauri Sankar

Melungtse reaches 7,181 meters, making it 47 meters higher than neighboring Gauri Sankar. Nevertheless, Gauri Sankar is much more familiar because it is prominently visible from Nepal.

The Mountain Has Several Names

The spelling Menlungtse appears frequently in historical expedition accounts, while Melungtse has become common in modern geographic databases.

The local Tibetan name recorded by early expeditions was Jobo Garu. Chinese-language sources have also used forms transliterated as Qiao Ge Ru or Qiáogérú Fēng.

Eric Shipton Helped Popularize the Name

Eric Shipton and Michael Ward entered the Menlung Valley in 1951 while returning from an Everest reconnaissance expedition. They called the mountain Menlungtse after the surrounding valley or pass, apparently without knowing its existing Tibetan name.

Famous “Yeti” Tracks Were Photographed Nearby

Shipton’s 1951 journey through the Menlung Valley became famous for photographs of unusual tracks in the snow.

The images are among the best-known pieces of supposed yeti evidence. However, they do not scientifically establish the existence of an unknown human-like Himalayan animal, and several ordinary-animal explanations have been proposed.

A Snow Leopard Surprised an Expedition

During the 1990 American expedition, John Roskelley reportedly encountered a snow leopard at close range while carrying supplies along a moraine.

The sighting provides a rare direct historical record of one of the Himalayas’ most elusive animals near the mountain.

The Western Summit Was Climbed First

Melungtse II was reached in 1988, four years before the first ascent of the higher main summit.

The western summit did not provide an easy route onward. A long, exposed ridge and the remaining elevation separated it from the main top.

The Main Summit Was Climbed by a Two-Person Team

Marko Prezelj and Andrej Štremfelj completed the first ascent of Melungtse’s main summit in 1992.

Their expedition was exceptionally small. The two climbers were accompanied at base camp by physician Žarko Guzej, but Prezelj and Štremfelj formed the active summit team.

The Successful Route Climbed a 2,000-Meter Face

The first-ascent route followed the southeast face, which rises approximately 2,000 vertical meters.

The climbers considered much of the technical climbing manageable by elite Himalayan standards, but the lower face was extremely dangerous because of falling stones, ice, and avalanches.

Melungtse Is an Ultra-Prominent Peak

Melungtse has approximately 1,550 to 1,570 meters of topographic prominence, depending on the database and elevation model used.

Because both commonly reported values exceed 1,500 meters, the mountain qualifies as an ultra-prominent peak.

The Mountain Remains Rarely Climbed

The 1992 ascent remains the only successful climb of the main summit consistently documented in the major mountaineering records consulted for this guide.

Later expeditions explored the north face but were stopped by heavy snowfall, avalanche danger, dangerous seracs, and a climber’s medical problem.

❓ Frequently Asked Questions

Where is Melungtse?

Melungtse is in Tingri County within the Tibet Autonomous Region of China. It stands just north of the Nepal–China border in the Rolwaling Himal.

Is Melungtse in Nepal or China?

The main summit is in China rather than Nepal. The wider Rolwaling Himal extends across the international border, and Melungtse can be viewed from some locations in Nepal, which sometimes causes confusion about its location.

How high is Melungtse?

Melungtse reaches 7,181 meters, or 23,560 feet, above sea level.

Is Melungtse the highest mountain in the Rolwaling Himal?

Yes. Melungtse is the highest summit of the Rolwaling Himal. Gauri Sankar is the second major 7,000-meter mountain most closely associated with the range.

Who made the first ascent of Melungtse?

Slovenian climbers Marko Prezelj and Andrej Štremfelj made the first confirmed ascent of the main summit on October 23, 1992.

They climbed the southeast face in alpine style and descended along the same general line.

When was Melungtse II first climbed?

Andy Fanshawe and Alan Hinkes reached the 7,023-meter western summit on May 23, 1988, during an expedition led by Chris Bonington.

A few later summaries give 1987, but detailed expedition reports clearly place the successful western-summit ascent during the 1988 expedition.

Has anyone traversed between the two summits?

There is no widely documented complete traverse connecting Melungtse II with the 7,181-meter main summit.

The ridge is approximately two kilometers long and includes exposed, corniced, and technically difficult terrain. The first ascents of the two summits were completed by different routes during separate expeditions.

Why is Melungtse less famous than Gauri Sankar?

Gauri Sankar is much more visible from populated areas and trekking routes in Nepal. It also holds strong cultural importance and has a distinctive twin-summited appearance.

Melungtse stands farther north and is partly hidden behind the main Himalayan ridges, despite being slightly higher.

Can ordinary trekkers visit Melungtse?

Ordinary trekkers can explore Nepal’s Rolwaling Valley and may obtain distant views of the massif, but they cannot trek directly to Melungtse’s Tibetan base camps from Nepal.

An approach to the mountain itself requires authorization for travel and climbing in Tibet, complicated expedition logistics, and highly experienced technical mountaineers.

Is there a normal climbing route?

No regularly climbed normal route exists.

The southeast-face route used for the first ascent is the only confirmed route to the main summit, but it is an extremely serious alpine climb exposed to rockfall, avalanches, icefall, altitude, and difficult retreat.

What is the best season for Melungtse?

The most practical Himalayan expedition periods are generally April through May and September through October.

Even during these seasons, severe storms, heavy snowfall, electrical activity, strong winds, and unstable snow may develop. Historical expeditions have been stopped in both spring and autumn.

Is Melungtse an ultra-prominent mountain?

Yes. Its estimated prominence exceeds the 1,500-meter threshold used to define an ultra-prominent summit.

What is Melungtse’s nearest higher neighbor?

The nearest higher terrain is associated with Nangpai Gosum I, also identified in some sources as Cho Aui. It stands approximately 21.2 kilometers east-northeast of Melungtse.

Is Melungtse suitable for commercial expeditions?

Melungtse is not an appropriate commercial expedition objective in the ordinary sense.

It lacks a repeatedly climbed standard route, and its faces involve exceptionally serious technical and objective hazards. Any future attempt would require a highly specialized team capable of operating independently on difficult Himalayan terrain.

🔗 Related Articles

• Mountains of Tibet
• Highest Mountains in China
• Mountains in China
• Mountains in Nepal
• Highest Mountains in Asia
• Mount Everest
• What Is Mountain Prominence?
• What Is an Ultra-Prominent Peak?
• Mountain Elevation vs. Prominence

Sources

• American Alpine Club — Menlungtse Attempt, 1987 Expedition — Account of the south-southwest buttress attempts, approach, terrain, storms, and climbing hazards. (AAC Publications)
• American Alpine Club — Menlungtse Western Summit — Detailed report of the May 23, 1988 first ascent of Melungtse II by Andy Fanshawe and Alan Hinkes. (AAC Publications)
• American Alpine Club — Menlungtse Attempt, 1990 — Greg Child’s account of the American southeast-ridge attempt and the snow-leopard encounter. (AAC Publications)
• American Alpine Club — Menlungtse, Rolwaling Himal — Andrej Štremfelj’s report of the 1992 first ascent of the main summit. (AAC Publications)
• American Alpine Club — Menlungtse Attempt and Milarepa Ascent — Report of the 1999 north-face attempt, heavy snowfall, and nearby Milarepa Peak ascent. (AAC Publications)
• American Alpine Club — Menlungtse North Face Attempt — Retrospective account of the 1999 and 2005 north-face expeditions. (AAC Publications)
• Himalayan Club — Menlungtse, 1987 — Chris Bonington’s account of the mountain, its names, early exploration, and the first major authorized attempt. (Himalayan Club)
• Himalayan Club — Menlungtse — Detailed expedition history, approach geography, valley vegetation, and first ascent of the western summit. (Himalayan Club)
• Peakbagger — Melungtse — Elevation, prominence, range classification, and surrounding summit relationships. (Peakbagger)
• Geosphere — The Geology of the Tama Kosi and Rolwaling Valley Region — Regional study of Greater Himalayan metamorphic rocks, structures, and tectonic history. (pubs.geoscienceworld.org)