Karjiang: The Himalayan Giant First Climbed in 2024

Karjiang (Karejiang)

Karjiang is a remote 7,000-meter mountain in southern Tibet, rising near the border between China and Bhutan. Its main summit reaches approximately 7,221 meters (23,691 feet), placing it among the world’s 100 highest mountains.

For decades, Karjiang was especially notable for another reason: it was one of the highest unclimbed mountains on Earth. Japanese and Dutch expeditions reached nearby summits but found the steep, avalanche-prone main peak too dangerous or technically difficult to complete.

That distinction finally ended on August 13, 2024, when Chinese climbers Liu Yang and Song Yuancheng reached the summit by a demanding new route on the southwest face. Their ascent transformed Karjiang from one of the Himalayas’ great unresolved challenges into the site of one of the most significant first ascents of the 2020s.

Karjiang remains an exceptionally serious mountain. It is remote, heavily glaciated, exposed to unstable weather, and far beyond the reach of ordinary trekkers. Even after its first ascent, only a very small number of climbers have stood on its summit.

🏔️ Overview

Karjiang is part of the high mountain complex surrounding Kula Kangri in the eastern Himalayas. It rises in the Tibet Autonomous Region of China, only a few kilometers north of the international border with Bhutan.

The name Karjiang is sometimes used for the entire cluster of neighboring summits rather than solely for the highest point. The principal summit is therefore frequently identified as Karjiang I, Karjiang South, or the South Peak.

The Karjiang group includes several significant summits:

Karjiang I or Karjiang South: approximately 7,221 m
Karjiang II or Central Peak: elevation figures vary among historical sources
Karjiang III or Taptol Kangri: approximately 6,824 m
Kangmi Kangri: approximately 6,412 m on the northeastern spur

Older expedition records are not completely consistent about the heights and numbering of the subsidiary summits. In particular, the name Karjiang II has been associated with different reported elevations. The main south summit, however, is widely accepted as the highest point of the group.

Karjiang’s proximity to the much larger Kula Kangri massif reduces its topographic independence, but not its visual or mountaineering importance. The mountain rises as a steep, sharply defined pyramid of ice, snow, rock, and hanging glaciers.

Before 2024, Karjiang was commonly described as the fourth-highest unclimbed independent mountain in the world, behind Gangkhar Puensum, Lapche Kang II, and Apsarasas Kangri I. Rankings vary according to the prominence threshold used to distinguish independent mountains from subsidiary summits.

The successful 2024 climb removed Karjiang from the unclimbed list, although nearby Gangkhar Puensum remains widely recognized as the world’s highest unclimbed mountain.

⚡ Fast Facts

Fact	Details
Continent	Asia
Country	China
State/Province	Tibet Autonomous Region
County/Region	Lhozhag County, Shannan or Lhoka
Mountain Range	Eastern Himalaya, Kula Kangri group
Parent Peak	Kula Kangri
Elevation	7,221 m / 23,691 ft
Prominence	Approximately 880 m / 2,887 ft
Isolation	Approximately 3 km / 1.9 mi
Nearest Higher Neighbor	Kula Kangri East, within the Kula Kangri massif
Coordinates	Approximately 28.2603° N, 90.6450° E
Main Summit	Karjiang I or Karjiang South
First Ascent	August 13, 2024
First Ascensionists	Liu Yang and Song Yuancheng
First-Ascent Route	Southwest Face
Route Name	Buzzer Beater
Route Grade	Approximately AI3, M4, 70° snow
Climbing Status	Climbed; at least two recorded ascents in 2024

📍 Location

Karjiang rises in Lhozhag County, part of Shannan—also known as Lhoka—in the southern Tibet Autonomous Region of China. The summit stands close to Bhutan, but available maps and modern geographic descriptions generally place the mountain itself north of the international border within Chinese-administered Tibet.

The mountain is approximately 165 kilometers southwest of Lhasa. Although that distance may not appear enormous on a map, the intervening Tibetan Plateau, restricted border region, high passes, glaciers, and limited transportation make the mountain difficult to approach.

Karjiang lies immediately northeast of Kula Kangri, one of the highest mountains in the eastern Himalayas. The two mountains form part of a compact concentration of extremely high summits overlooking the Tibetan–Bhutanese frontier.

Depending on the exact summits being measured, Karjiang is only about three kilometers from the nearest higher part of the Kula Kangri massif. This close relationship explains Karjiang’s relatively modest isolation despite its enormous elevation.

The Kula Kangri Group

The broader Kula Kangri mountain complex contains several peaks exceeding 7,000 meters. The principal Kula Kangri summit reaches approximately 7,538 meters, although older references sometimes report different elevations for its main and subsidiary summits.

Karjiang rises northeast of this massif as a distinct mountain separated from the neighboring higher peaks by a deep saddle. Its approximately 880 meters of prominence is enough for many mountain-ranking systems to treat it as an independent mountain rather than merely another summit of Kula Kangri.

The surrounding landscape includes:

Extensive valley glaciers
High snowfields
Moraines and glacial debris
Steep ice faces
Hanging seracs
Narrow ridges
Sparsely inhabited Tibetan valleys

The mountain’s northern glaciers drain toward the interior of the Tibetan Plateau. Meltwater from the surrounding ranges also contributes to high-altitude lakes and rivers in the region.

Pumo Yumco

About 30 kilometers north of Karjiang lies Pumo Yumco, a striking high-altitude lake on the Tibetan Plateau. The lake stands at roughly 5,000 meters above sea level and receives meltwater from surrounding snowfields and glaciers.

On clear days, Karjiang and the neighboring Kula Kangri summits can be seen beyond the lake, forming one of the most dramatic mountain skylines in southern Tibet.

The lake’s name is commonly translated as the “blue jewel floating in the sky,” an appropriate description of its deep blue water and elevated plateau setting.

A Remote Border Mountain

Karjiang is not located within a developed trekking destination comparable to the Everest, Annapurna, or Langtang regions of Nepal. Access is shaped by Chinese travel regulations, mountaineering permissions, border restrictions, weather conditions, and the availability of local transportation and logistical support.

International climbers have historically found it difficult to obtain permission for expeditions to Karjiang. Even experienced teams that received preliminary support or funding were not always able to secure the final permits required to reach the mountain.

The remoteness has contributed to Karjiang’s limited climbing history. It has also helped preserve the surrounding valleys as one of the quieter and less frequently documented parts of the high Himalayas.

🏔️ Field Guide Tip: Karjiang should not be treated as a conventional hiking or trekking destination. Independent travel in this sensitive border region may be restricted, and any expedition would require current permits, experienced local assistance, high-altitude climbing skills, and specialized glacier equipment.

📏 Elevation & Prominence

Karjiang’s generally accepted elevation is 7,221 meters, equivalent to 23,691 feet. Some mountaineering reports and historical records use a figure of approximately 7,216 meters, partly because of inconsistencies involving the main summit and nearby Karjiang II.

For general geographic and mountain-ranking purposes, 7,221 meters remains the most widely used elevation for Karjiang’s main south summit.

How High Does Karjiang Rank?

Karjiang is often listed between approximately the 97th and 100th highest mountains in the world. Its precise position depends on how a ranking treats subsidiary summits, disputed elevations, prominence, and closely connected neighboring peaks.

Mountaineering statistician Eberhard Jurgalski has listed Karjiang as the 97th-highest mountain in the world under a system that distinguishes principal mountains from subsidiary tops.

Other lists place it slightly lower. It is therefore safest to describe Karjiang as one of the world’s 100 highest mountains rather than assigning it a universal rank.

Karjiang is lower than nearby Kula Kangri by approximately 317 meters. Nevertheless, it remains higher than many better-known Himalayan mountains and exceeds the 7,000-meter threshold by more than 200 meters.

Prominence

Karjiang has a topographic prominence of approximately 880 meters, or about 2,887 feet.

Topographic prominence measures how far a climber must descend from a summit before reaching terrain connected to a higher mountain. Karjiang’s key saddle links it to the neighboring Kula Kangri massif.

Some topographic datasets report a prominence closer to 895 meters. This small difference likely reflects variations in elevation models and the calculated height of the connecting saddle.

Although Karjiang does not meet the 1,500-meter prominence standard required to qualify as an ultra-prominent peak, 880 meters is substantial enough for the mountain to possess a strong independent identity.

Isolation

Karjiang’s topographic isolation is only about three kilometers, or slightly less than two miles. Its nearest higher terrain is associated with an eastern summit of the Kula Kangri massif.

This short isolation distance does not mean that Karjiang is a minor peak. Instead, it reflects the extraordinary concentration of high mountains in the region. A 7,221-meter summit can have limited isolation when an even higher 7,000-meter mountain rises immediately beside it.

Karjiang’s combination of great elevation, moderate prominence, and limited isolation demonstrates why mountain rankings can vary. Elevation measures absolute height above sea level, while prominence and isolation measure a summit’s relationship to the surrounding landscape.

🪨 Geology

Detailed peak-specific geological studies of Karjiang are limited in readily available sources. Its broader geological setting, however, is part of the well-documented formation of the Higher Himalaya and southern Tibetan Plateau.

Karjiang ultimately owes its existence to the collision between the Indian and Eurasian tectonic plates.

Formation of the Himalayas

The Indian Plate was once separated from Eurasia by the Tethys Ocean. As India moved northward, the ocean gradually closed, and the continental landmass collided with Eurasia approximately 50 million years ago.

Because continental crust is relatively buoyant, it did not simply sink into the mantle. Instead, enormous sections of rock were compressed, folded, faulted, stacked, and pushed upward.

This process produced:

The Himalayan mountain chain
The uplifted Tibetan Plateau
Major thrust faults
Thickened continental crust
Intense metamorphism
Widespread granite intrusions

The collision is continuing today. Southern Tibet and the Himalayas remain tectonically active, with ongoing crustal deformation, uplift, fault movement, and earthquakes.

Regional Rock Types

The Higher Himalaya contains large bodies of metamorphic and igneous rock. Common regional rocks include:

Gneiss
Schist
Quartzite
Metamorphosed sedimentary rocks
Granite
Leucogranite

Gneiss and schist formed as older rocks were buried, heated, compressed, and transformed during Himalayan mountain building. Younger granitic bodies developed when portions of the thickened continental crust partially melted and magma rose into the surrounding rock.

Without detailed mapping of the summit pyramid, it would be speculative to assign one precise rock type to every part of Karjiang. The mountain is also so heavily covered by snow and ice that much of its underlying geology is concealed.

Glacial Sculpting

Tectonic uplift created Karjiang’s great height, but glaciers helped shape its present appearance.

Repeated glacial advances carved the surrounding valleys and sharpened the mountain’s ridges. Ice flowing away from the massif transported broken rock downhill, creating extensive moraines below the mountain.

Freeze-thaw weathering continues to fracture exposed rock. Water enters cracks during warmer periods, freezes as temperatures fall, expands, and gradually breaks the rock apart. This process contributes to the loose mixed terrain encountered near the summit.

Karjiang’s steep faces also support hanging glaciers and seracs—large, unstable blocks or towers of glacial ice. These features are among the mountain’s greatest hazards because they can collapse with little warning.

Snow accumulation, avalanches, glacier movement, and rockfall constantly reshape the mountain. Karjiang is therefore not a static landform but part of an active landscape in which geological uplift and surface erosion continue simultaneously.

🌿 Flora & Fauna

Karjiang rises far above the elevation at which trees, shrubs, or continuous plant communities can survive. Its upper slopes consist almost entirely of snow, exposed rock, and glacial ice, creating one of the harshest environments in the eastern Himalayas.

The summit itself lies within the permanent high-alpine and nival zone. Temperatures remain below freezing for much of the year, oxygen levels are extremely low, and powerful winds prevent meaningful soil development. No vascular plants are expected to grow on the mountain’s upper faces or summit ridge.

Conditions become more hospitable farther down the approach valleys. The lower slopes and plateau surrounding the Karjiang and Kula Kangri groups contain areas of alpine grassland, sparse steppe vegetation, rocky tundra, glacial outwash, and seasonal wetlands.

Plant Life

Vegetation around Karjiang varies according to elevation, slope direction, moisture, snow cover, and exposure to wind.

The most likely plant communities in the lower valleys include:

Cold-tolerant alpine grasses
Sedges
Low cushion plants
Small flowering herbs
Mosses
Lichens
Sparse plants growing between rocks
Wetland vegetation near streams and lakes

The short growing season usually begins after snowmelt and lasts only through the warmer summer months. Plants must reproduce quickly before temperatures fall again.

Many high-altitude plants remain close to the ground, where they receive some protection from wind. Their compact growth forms also help conserve heat and moisture.

Above approximately 5,500 to 6,000 meters, vegetation becomes extremely limited. Only lichens, microorganisms, or isolated patches of exceptionally hardy plant life may survive on protected rock surfaces. Karjiang’s climbing routes begin near or above this elevation and pass almost entirely through a lifeless world of ice and stone.

The wider Tibetan Plateau contains the world’s largest area of alpine grassland. These grasslands are ecologically important because they stabilize soil, store carbon, provide habitat for wildlife, and support the pastoral communities that graze yaks, sheep, and goats in the lower valleys.

Wildlife of the Region

There are few detailed biological surveys focused specifically on Karjiang. Wildlife associated with the surrounding southern Tibetan Plateau may include species adapted to cold, dry, high-altitude environments.

Possible regional mammals include:

Himalayan or Tibetan blue sheep
Plateau pikas
Himalayan marmots
Tibetan foxes
Tibetan wolves
Snow leopards
Weasels and other small carnivores

This does not mean that every species has been documented directly on Karjiang. The mountain’s extreme elevation, steep glaciers, and limited human access have prevented comprehensive wildlife surveys.

Blue sheep are among the most important large herbivores in high Himalayan and Tibetan ecosystems. Their gray-brown coats provide camouflage among rocky slopes, while their specialized hooves allow them to travel across steep terrain.

Snow leopards occupy remote mountain landscapes across High Asia and prey heavily on wild sheep and goats. The rugged valleys around the Tibet–Bhutan border may provide suitable habitat, although the cats are secretive and rarely observed.

Plateau pikas and marmots are more likely to be encountered in grasslands below the glaciers. Pikas create burrow systems and serve as prey for foxes, wolves, raptors, and other predators. Their burrowing also affects vegetation and soil structure.

Birds

Birdlife is more visible around the valleys, cliffs, and high-altitude lakes than on Karjiang’s glaciated summit slopes.

Species potentially found in the wider region include:

Himalayan griffons
Lammergeiers or bearded vultures
Golden eagles
Ravens
Snow pigeons
Horned larks
Accentors
High-altitude waterbirds

Large raptors use rising air currents to travel efficiently over the plateau. Ravens may also investigate campsites, especially where food or waste has been left exposed.

Pumo Yumco and other lakes of southern Tibet provide seasonal habitat for waterbirds. The lake environment is ecologically distinct from Karjiang’s glaciated slopes but forms part of the same regional landscape.

Domestic Animals

Yaks, Tibetan sheep, goats, horses, and pack animals have long supported communities on the Tibetan Plateau. Expeditions may depend on horses, donkeys, yaks, or local porters to transport supplies toward base camp.

Pack animals normally cannot travel onto the upper glaciers. During Karjiang’s 2024 first-ascent expedition, the porters stopped at approximately 5,800 meters, forcing the climbers to establish base camp lower than they had originally planned.

Domestic livestock can be important to local livelihoods, but heavy grazing may also damage fragile alpine vegetation. Recovery is slow because plants grow only during a short summer season.

🏔️ Field Guide Tip: Visitors should carry out all waste, including food scraps and damaged equipment. Cold, dry high-altitude environments decompose organic material very slowly, and abandoned waste may remain visible for decades.

🥾 Hiking & Climbing Routes

Karjiang has no ordinary hiking trail or nontechnical route to its summit. Every known line requires expedition-level mountaineering, glacier travel, avalanche assessment, mixed climbing, and prolonged exposure above 6,000 meters.

The mountain should be considered an objective for highly experienced high-altitude alpinists rather than hikers or recreational climbers.

As of 2026, only two successful ascents of Karjiang’s main summit have been publicly documented. Both followed the southwest face, although the second team used a somewhat more direct variation.

The Northern Glacier Approach

Recorded expeditions have approached Karjiang from the Tibetan side, traveling southward toward the glaciers flowing from the Karjiang and Kula Kangri groups.

The precise approach may vary according to road conditions, permits, glacier changes, and the chosen base-camp location. Climbers must generally cross:

Remote plateau terrain
Glacial streams
Moraines
Loose debris
Crevassed glaciers
Snow-covered ice
High camps exceeding 5,500 meters

During the 2024 expedition, the team reached a base camp at approximately 5,800 meters after trekking up the glacier north of Karjiang. The site was lower than the climbers preferred because their porters were unwilling or unable to continue farther.

An approach camp at this height is already higher than the summits of many major mountains. Climbers must therefore complete much of their acclimatization before attempting the face.

Southwest Face: Buzzer Beater

The first successful route on Karjiang was established by Chinese climbers Liu Yang and Song Yuancheng in August 2024.

They named the route Buzzer Beater because the ascent was completed near the end of the limited time available before they had to leave Tibet.

The route is approximately 1,300 meters high and was graded:

AI3 for alpine ice
M4 for mixed rock-and-ice climbing
Up to 70 degrees on snow slopes

Grades alone do not fully represent the climb’s seriousness. The greatest difficulties included deep snow, unstable mixed terrain, poor protection, seracs, bad visibility, extreme altitude, and the absence of an easy descent.

First Attempt in 2024

Liu and Song began their first attempt on July 31, 2024. They climbed the southwest face and established their first camp beneath a serac at approximately 6,350 meters.

The following day, they continued to around 6,650 meters and again bivouacked beneath a serac. A storm then deposited about one meter of new snow overnight.

Despite the snowfall, they climbed approximately another 250 meters before spending two hours cutting a platform large enough for their tent.

Continued snow, headaches, and deteriorating conditions forced them to retreat. Their experience nevertheless confirmed that the face might be climbable during a sufficiently long weather window.

First Ascent

After resting and reassessing the forecasts, Liu and Song returned to base camp on August 10. They began their decisive attempt at 2:30 a.m. on August 11 and reached the base of the southwest face at approximately 5:00 a.m.

This time, they selected a line nearer the rock wall to the left of their previous route.

The lower section consisted of relatively comfortable alpine ice. Higher up, the climbers encountered deep snow that made progress slower and more strenuous.

They reached approximately 6,550 meters and discovered a small natural ice cave. The space was too confined for their tent, so they bivouacked beneath the tent fly.

Snow fell overnight but stopped early on August 12. The climbers continued to a large crevasse beneath a serac at approximately 6,900 meters.

Their tent poles broke in the cold, once again leaving them to sleep beneath the flysheet rather than inside a properly erected tent.

Shortly after midnight on August 13, Liu and Song continued toward the summit. They left most of their equipment at the bivouac and climbed approximately 100 meters to loose mixed ground.

The terrain offered unreliable protection and required careful movement over snow, ice, and unstable rock.

At around 2:00 p.m., they finally reached the summit ridge. Turning right, they moved together along the crest for approximately 55 minutes before arriving at Karjiang’s highest point.

After decades of failed attempts, Karjiang had finally been climbed.

The Descent

Reaching the summit completed only half the challenge. Liu and Song began descending in a whiteout and struggled to relocate suitable rappel anchors.

Unable to find solid ice for their first rappel, they buried a pack lid in the snow and used it as an emergency anchor.

They then completed four rappels from Abalakov anchors cut into thin ice. Difficult downclimbing returned them to their high bivouac beneath the serac.

Although exhausted, the climbers decided not to remain there. They continued descending through snowfall and poor visibility while spindrift avalanches repeatedly swept across the face.

They reached the glacier at approximately 5:00 a.m. on August 14.

More than half a meter of snow had accumulated on the moraine below. The snow-covered boulders were so difficult and dangerous to cross that the climbers were sometimes forced to crawl.

It took them four and a half hours to cover approximately 1.5 kilometers between the glacier and base camp.

Second Ascent

Karjiang’s second ascent took place only about one month after the first.

Chinese mountain guides Huang Siyuan and Tong Zhanghao established an advanced base at approximately 5,900 meters and rested for one day. They began climbing at 3:30 a.m. on September 9, 2024.

Their route followed the southwest face but used a slightly more direct line than Buzzer Beater.

By approximately 1:00 p.m., they had reached a planned bivouac at 6,900 meters. Because they were ahead of schedule, they stopped for an open bivouac and rested until around midnight.

Deep, soft snow slowed their final summit push. Nevertheless, the pair reached the top shortly before 4:00 a.m. on September 10 and descended later that day.

Their climb was completed as a two-day round trip from the foot of the face.

The second ascent demonstrated that Karjiang’s southwest face could be climbed more quickly under comparatively stable post-monsoon conditions. It did not establish the mountain as an accessible or repeatable objective. The face continued to present severe avalanche, serac, altitude, and weather hazards.

🧗 Earlier Expeditions and Attempts

Karjiang remained unclimbed for so long because it combines technical difficulty with unusually complicated access.

Only a handful of serious attempts were recorded before 2024.

Japanese Expedition of 1986

A Japanese expedition attempted Karjiang’s main summit in 1986. The climbers considered the principal peak too difficult and instead turned toward the neighboring central or northern summit.

They reached Karjiang II by its northwest ridge.

Historical descriptions of the Karjiang summits are inconsistent. Some sources identify the 1986 summit as Karjiang II, the Central Summit, or the North Summit, and reported elevations vary.

The important distinction is that the Japanese expedition did not reach the highest point now generally called Karjiang I or Karjiang South.

This confusion contributed to occasional claims that Karjiang had already been climbed. Later mountaineering records continued to treat the 7,221-meter south summit as unclimbed until 2024.

Dutch Expedition of 2001

A six-member Dutch expedition arrived during the post-monsoon season in September 2001. The team consisted of Rudolf van Aken, Pepijn Bink, Court Haegens, Willem Horstmann, Rein-Jan Koolwijk, and Haroen Schijf.

They established base camp north of the Karjiang group on September 20 at approximately 4,950 meters.

The climbers initially investigated a possible northeastern route. From a col at around 5,800 meters, they obtained what may have been the first close mountaineering view of Karjiang’s northeast face.

They estimated the face to be at least 800 meters high. It appeared extremely steep, technically difficult, and exposed to serious objective danger. The team decided not to attempt it.

The climbers then moved to the opposite side of the mountain to investigate the west face.

They established another advanced base at approximately 5,700 meters and placed a high camp near 6,300 meters, close to the bottom of the face and below the col between Karjiang and Kula Kangri East.

Four climbers began ascending the west face. At approximately 6,550 meters, they triggered a slab avalanche more than 25 meters wide.

The slab fell roughly 200 meters down the face. No one was injured, but the incident indicated that the surrounding snowpack was dangerously unstable.

The team rappelled down the 55- to 60-degree face using snow anchors and Abalakov anchors. They subsequently examined the south ridge but rejected it because of heavy cornices and unsafe conditions.

Although they did not climb Karjiang’s main summit, the expedition made the first ascents of two neighboring peaks.

Taptol Kangri

On October 19, Pepijn Bink, Willem Horstmann, Rein-Jan Koolwijk, and Haroen Schijf climbed the approximately 6,824-meter northwest summit by its north face and west ridge.

The team named it Taptol Kangri, and it is now commonly identified as Karjiang III.

Their route climbed a roughly 500-meter face averaging approximately 50 degrees, with short sections approaching 55 degrees. The expedition assigned it an Alpine grade of D.

Kangmi Kangri

Rudolf van Aken and Court Haegens climbed a separate 6,412-meter summit on October 21.

After crossing a large bergschrund, they climbed a 55-degree ice face and followed a narrow ridge that included unstable snow slopes of up to approximately 65 degrees.

They named the mountain Kangmi Kangri, translated in the expedition report as “Yeti Snow Mountain.”

These subsidiary ascents added valuable geographic and climbing information about the previously little-known Karjiang group.

Permit Difficulties

Several proposed Karjiang expeditions never reached the mountain because permission was denied, delayed, or otherwise unavailable.

Southern Tibet contains politically sensitive border areas, and mountaineering regulations may change without warning. Receiving initial support for an expedition does not necessarily guarantee final access to the mountain.

The long gap between the 2001 attempt and the 2024 ascent was therefore not caused solely by climbing difficulty. Restricted access and the expense of organizing a remote Tibetan expedition also played important roles.

⚠️ Major Climbing Hazards

Karjiang presents nearly every major hazard associated with high-altitude Himalayan climbing.

Avalanches

Avalanches are among the mountain’s greatest dangers.

The 2001 Dutch expedition retreated after triggering a large slab avalanche on the west face. The 2024 first ascensionists encountered deep snow, repeated overnight accumulation, and spindrift avalanches during their descent.

The southwest face is steep enough to hold and release significant quantities of snow. Snow stability may change rapidly after storms, strong winds, or sudden warming.

Seracs

Large seracs rise above portions of the southwest face. Both 2024 teams used bivouac sites beneath or near seracs, largely because the terrain offered few alternatives.

Seracs can collapse without warning. Even experienced climbers cannot reliably predict the exact timing of an icefall.

Camping beneath one may provide shelter from wind or snowfall while increasing exposure to falling ice.

Crevasses

The approach glacier and upper face contain crevasses that may be hidden beneath fresh snow. The 2024 climbers used a large crevasse beneath a serac as their high bivouac site.

Crevasse rescue at elevations approaching 7,000 meters is exceptionally difficult because rescuers are already weakened by low oxygen and cold.

Cornices

The south ridge inspected in 2001 was heavily corniced. Cornices may extend far beyond the supporting rock or ice beneath them, making the apparent ridge crest unsafe.

A climber can break through a cornice even when walking on terrain that appears solid.

Loose Mixed Terrain

Near the summit ridge, the first ascensionists encountered loose mixed ground with poor opportunities for protection.

Rock weakened by freeze-thaw cycles may break when loaded. Snow-covered rock can also conceal loose holds and make route-finding difficult.

Extreme Altitude

Karjiang’s summit rises well into what mountaineers call the death zone, usually considered the area above 8,000 meters only in the strictest usage, but severe physiological deterioration begins far below that elevation.

At 7,000 meters, climbers experience:

Greatly reduced oxygen availability
Slow movement
Impaired judgment
Loss of appetite
Dehydration
Headaches
Poor sleep
Reduced coordination
Increased risk of altitude illness

The 2024 first ascensionists experienced headaches during their initial attempt and chose to retreat. That decision likely prevented a more serious emergency.

Cold and Wind

During the 2001 expedition, temperatures near the high camps fell to approximately −25°C, while extremely strong winds forced the team to retreat from a neighboring objective.

High winds can increase frostbite risk, destroy tents, remove snow from some slopes, and deposit dangerous wind slabs on others.

The first ascent team also experienced tent-pole failure caused by cold conditions.

Whiteouts

Karjiang is difficult to navigate when cloud and snowfall obscure the surrounding terrain.

Liu and Song began their summit descent in a whiteout and could not immediately find suitable rappel ice. On a rarely climbed mountain, there are no established anchors, wands, or tracks to guide the descent.

Remoteness

No rapid professional rescue system should be assumed to exist on Karjiang.

An injured climber may need to descend the technical face, cross a glacier, traverse unstable moraines, and travel through a restricted region before reaching advanced medical care.

Expedition teams must be prepared for self-rescue and prolonged evacuation.

🏔️ Field Guide Tip: Success on Karjiang depends as much on knowing when to retreat as on technical ability. Deep new snow, recent avalanche activity, unstable wind slabs, altitude symptoms, or an inadequate weather window should be treated as reasons to descend rather than challenges to push through.

🌤️ Best Time to Visit

Karjiang does not yet have a well-established climbing season. With only two documented ascents of its main summit, there is not enough experience to identify a consistently safe or reliable period.

Historical expeditions suggest that the post-monsoon months offer the most promising conditions, but every season presents serious disadvantages.

Summer: July and August

July and August coincide with the Asian summer monsoon. Although southern Tibet is drier than the Himalayan slopes farther south, moisture can still bring:

Persistent cloud
Heavy snowfall at high elevation
Poor visibility
Unstable snow
Spindrift avalanches
Difficult glacier travel

Liu Yang could attempt Karjiang only during his university summer vacation. The 2024 account specifically described July and August as less than ideal for this mountain.

During the first attempt, approximately one meter of snow fell overnight. Even on the successful climb, the team experienced repeated snowfall and poor visibility.

Their success depended on locating a narrow weather window rather than on generally favorable seasonal conditions.

Early Autumn: September

September currently appears to offer the strongest evidence for comparatively favorable climbing conditions.

The second ascent was completed in early September 2024 during more stable post-monsoon weather. The team climbed more quickly than the first ascensionists and completed the route in a two-day round trip.

However, deep and soft snow remained present near the summit. September should not be interpreted as reliably dry or safe.

Storms can still reach the mountain, while shorter days and colder nights become increasingly important later in the month.

Late Autumn: October

October may bring clearer skies but also colder temperatures and stronger winds.

During the Dutch expedition in October 2001, temperatures fell to approximately −24°C to −25°C. Strong winds and unstable snow affected several of the team’s objectives.

The tradeoff is therefore significant: reduced monsoon influence may improve visibility, but colder and windier conditions can make climbing equally dangerous.

Spring

Spring is a traditional expedition season on many Himalayan mountains, but Karjiang has too little recorded climbing history to define a reliable spring window.

Potential advantages might include longer daylight than in late autumn and gradual seasonal warming. Potential disadvantages include:

Heavy winter snow remaining on the mountain
Unstable spring snow
High winds
Cornice development
Closed or difficult approach routes
Uncertain permit availability

Any spring expedition would require recent satellite imagery, local observations, and careful assessment of the glacier and snowpack.

Winter

Winter would bring extreme cold, short daylight hours, intense wind, and highly demanding logistical conditions.

No winter ascent of Karjiang has been documented. Given the mountain’s remoteness and technical difficulties, a winter attempt would represent a major exploratory undertaking rather than a conventional expedition.

Permits and Access

The theoretical best climbing season is irrelevant unless access is legally available.

Karjiang lies in a sensitive area near the Bhutan–China border. Climbers must verify current regulations through authorized Chinese and Tibetan mountaineering organizations.

Requirements may include:

A Chinese visa
A Tibet Travel Permit
A mountaineering permit
Approval for travel in a restricted border area
A registered local operator
Liaison staff
Transportation authorizations
Environmental fees
Rescue and evacuation plans

Regulations can change, and historical permission does not guarantee that future expeditions will be approved.

For most travelers, the more realistic way to experience the Karjiang region would be from an authorized route or viewpoint near Pumo Yumco rather than from the mountain itself.

🧭 Nearby Mountains & Attractions

Karjiang occupies one of the most remote and least frequently visited corners of the eastern Himalayas. Its closest surroundings are dominated by glaciers, high passes, unnamed ridges, and other major summits rather than towns or developed visitor attractions.

Access to the region may be restricted, especially because Karjiang lies near the China–Bhutan border. The nearby places described below should therefore be understood primarily as geographic features rather than easily accessible tourist destinations.

Kula Kangri

Kula Kangri is Karjiang’s parent mountain and its closest major neighbor. Its summit stands only about three kilometers southwest of Karjiang.

Published elevations for Kula Kangri range from approximately 7,538 to 7,554 meters. The variation reflects differences among historical surveys, maps, and mountaineering records rather than any uncertainty that Kula Kangri is significantly higher than Karjiang.

The Kula Kangri massif contains several high summits:

Kula Kangri Main
Kula Kangri Central
Kula Kangri East
Several smaller subsidiary tops and connecting ridges

A Japanese expedition completed the first ascent of the main Kula Kangri summit in 1986. Its east and central summits were climbed by another Japanese expedition in 2002.

Karjiang is connected topographically to the Kula Kangri group by a high saddle. This relationship explains why Kula Kangri is considered Karjiang’s parent peak and nearest higher mountain.

Karjiang Northwest

A high subsidiary summit rises immediately northwest of Karjiang’s main peak. Modern topographic compilations commonly assign it an elevation of approximately 7,216 meters.

A Japanese expedition led by Nobuhiro Shingo reached this summit in October 1986 after deciding that Karjiang’s higher south summit was too difficult. Nobuhiro Shingo, Kenji Tomoda, and Hiroshi Iwasaki reached the top on October 14, followed by Tsutomu Miyazaki and Akinori Hosaka on October 16.

Historical accounts called the summit Karjiang II or the Central Summit. More recent descriptions sometimes distinguish the 7,216-meter northwest summit from a separate central summit of approximately 7,045 meters.

This inconsistent naming is one of the greatest sources of confusion in Karjiang’s climbing history.

Karjiang III or Taptol Kangri

Karjiang III, also known as Taptol Kangri, rises northwest of the main summit. Its generally reported elevation is approximately 6,824 meters.

Pepijn Bink, Willem Horstmann, Rein-Jan Koolwijk, and Haroen Schijf made its first recorded ascent on October 19, 2001. They climbed a roughly 500-meter north face before following a snow-covered west ridge to the summit.

The climbers graded the route Alpine D and named the mountain Taptol Kangri after consulting people from the surrounding region.

Although considerably lower than Karjiang’s main summit, Taptol Kangri is still higher than the highest mountains of North America, Europe, Africa, and Antarctica.

Kangmi Kangri

Kangmi Kangri is a roughly 6,412-meter summit on the northeastern side of the Karjiang group.

Rudolf van Aken and Court Haegens completed its first recorded ascent on October 21, 2001. Their route crossed a large bergschrund, climbed a 55-degree ice face, and continued along a narrow ridge containing sections of unstable snow.

The climbers named the summit Kangmi Kangri, translated in their expedition account as “Yeti Snow Mountain.”

Kangmi Kangri is sometimes described as a subsidiary summit or shoulder of the Karjiang group rather than a completely independent mountain.

Gangkhar Puensum

Gangkhar Puensum rises approximately 30 kilometers southwest of Karjiang. It stands on or close to the disputed boundary between Bhutan and China.

With an elevation generally reported between approximately 7,570 and 7,575 meters, Gangkhar Puensum is widely regarded as the world’s highest unclimbed mountain.

Its unclimbed status is partly connected to Bhutan’s restrictions on high-altitude mountaineering. Bhutan prohibited climbing mountains above 6,000 meters in 1994 and later introduced a broader mountaineering ban.

Before Karjiang’s first ascent, Gangkhar Puensum, Lapche Kang II, and Apsarasas Kangri I were the only unclimbed independent mountains ranked above it under Eberhard Jurgalski’s classification system.

Chura Kang

Chura Kang is another high summit associated with the mountainous Bhutan–Tibet frontier.

The mountain lies south of the Karjiang and Kula Kangri groups. Its precise elevation and political location vary among maps, partly because the international boundary in this region has not been fully resolved.

Chura Kang is less well known internationally than Karjiang or Gangkhar Puensum, but it forms part of the same remote concentration of eastern Himalayan summits.

Jiexiang Group

The Jiexiang Group is a collection of high summits visible west of the Karjiang and Kula Kangri massifs.

A photograph accompanying the 2025 American Alpine Journal report identifies the group’s highest point at approximately 6,672 meters and describes it as unclimbed at the time of publication.

The limited information available about the Jiexiang peaks demonstrates how much of southern Tibet remains poorly documented in the international mountaineering record.

Pumo Yumco

Pumo Yumco—also written Puma Yumco—is a large high-altitude lake approximately 30 kilometers north of Karjiang.

The lake lies at approximately 5,000 meters above sea level. Its blue water, surrounding brown plateau, and distant snow-covered mountains create one of the region’s most remarkable landscapes.

On clear days, the Karjiang and Kula Kangri groups can be seen across the lake. A photograph published with the first-ascent account identifies Karjiang, Karjiang II, three Kula Kangri summits, and the Jiexiang Group along the southern horizon.

Pumo Yumco freezes during winter. NASA observations have also documented changes in the lake’s size, with water levels influenced by precipitation and regional climatic conditions.

Travel around the lake may still require permits and an authorized itinerary. Visitors should not assume that seeing the mountains from Pumo Yumco means that they can independently continue toward Karjiang’s base camp.

🏔️ Field Guide Tip: Pumo Yumco offers a much more realistic way for travelers to see the Karjiang and Kula Kangri groups than attempting to enter the glaciers below the mountains. Visibility depends heavily on cloud, snowfall, dust, and seasonal weather.

Lhasa

Lhasa lies approximately 165 kilometers northeast of the Karjiang and Kula Kangri groups. Despite the relatively modest straight-line distance, travel between Lhasa and the mountain requires crossing a vast area of high plateau.

Expeditions commonly use Lhasa as a logistical and acclimatization base. The 2024 first-ascent team returned to the city between its initial reconnaissance, unsuccessful attempt, and successful summit climb.

Lhasa is also the principal transportation center for most authorized journeys through the Tibet Autonomous Region.

💡 Fun Facts

Karjiang Was One of the Highest Unclimbed Mountains

Before August 2024, Karjiang was commonly described as the world’s fourth-highest unclimbed independent mountain.

Only Gangkhar Puensum, Lapche Kang II, and Apsarasas Kangri I ranked above it under the system cited by the American Alpine Journal.

It May Be the World’s 97th-Highest Mountain

Mountaineering statistician Eberhard Jurgalski ranks Karjiang as the world’s 97th-highest independent mountain.

Other lists place it around 99th because mountain rankings change according to which subsidiary summits are counted. It is best described more broadly as one of the 100 highest mountains on Earth.

The Main Summit Was Rejected in 1986

The first expedition known to make a serious attempt on Karjiang’s main summit concluded that it was too difficult.

The Japanese climbers changed objectives and instead reached the neighboring 7,216-meter summit.

A Dutch Team Triggered an Avalanche

During the 2001 attempt, four climbers reached approximately 6,550 meters on Karjiang’s west face before triggering a slab avalanche more than 25 meters wide.

The slab traveled about 200 meters down the face. No one was injured, but the team immediately abandoned the route.

The First-Ascent Route Was Named Buzzer Beater

Liu Yang and Song Yuancheng named their route Buzzer Beater because they completed the climb immediately before they had to leave Tibet.

After reaching base camp on August 14 and traveling through the night, they arrived in Lhasa early on August 15, shortly before their scheduled flights.

The First Ascensionists Used a Pack Lid as an Anchor

While descending in a whiteout, Liu and Song could not find suitable ice for a rappel anchor.

They buried the lid of a backpack in the snow and used it as an emergency anchor before reaching terrain where they could construct Abalakov ice anchors.

Their Tent Failed High on the Mountain

At their approximately 6,900-meter bivouac, the first-ascent team’s tent poles broke in the cold.

The climbers spent the night beneath the tent fly before beginning their summit push shortly after midnight.

The Second Ascent Followed Only One Month Later

Huang Siyuan and Tong Zhanghao made Karjiang’s second recorded ascent in September 2024, only about four weeks after the first.

They climbed a slightly more direct variation of the southwest face and completed a two-day round trip from the foot of the route.

The Mountain Has Confusing Summit Names

Different expeditions have used the names Karjiang North, Karjiang Northwest, Karjiang Central, and Karjiang II for different high points.

Even authoritative mountaineering records do not use a completely consistent system. Elevations should therefore always be paired with a summit description when discussing Karjiang’s subsidiary peaks.

The Summit Is More Than Two Kilometers Above Base Camp

The 2024 first-ascent expedition established base camp at approximately 5,800 meters.

Karjiang’s summit rises more than 1,400 vertical meters above that camp, while the climbed southwest face itself is approximately 1,300 meters high.

Karjiang Was First Climbed During the Monsoon

July and August are not considered ideal months for Karjiang because summer monsoon moisture can bring deep snow and poor visibility.

Liu Yang’s work as a university lecturer limited him to the summer holidays, so the team succeeded during a season that had discouraged other potential expeditions.

❓ Frequently Asked Questions

Where is Karjiang?

Karjiang is in the Tibet Autonomous Region of China, close to the international border with Bhutan. It rises within the eastern Himalayas, immediately northeast of the Kula Kangri massif.

How high is Karjiang?

Karjiang’s accepted elevation is approximately 7,221 meters, or 23,691 feet.

Some climbing reports label the climbed summit as 7,216 meters, reflecting continuing uncertainty and confusion surrounding the elevations and names of the group’s closely spaced summits. The 7,221-meter figure remains the standard elevation for Karjiang I or Karjiang South.

Is Karjiang in China or Bhutan?

Available coordinates and modern geographic references place Karjiang’s main summit within the Tibet Autonomous Region of China, north of the Bhutanese border.

Some general descriptions call it a border mountain because it stands extremely close to Bhutan. This does not necessarily mean that the summit lies directly on the international boundary.

Has Karjiang been climbed?

Yes. Karjiang’s main summit was first climbed on August 13, 2024.

A second team reached the summit on September 10, 2024. Both successful parties climbed the southwest face.

Who made the first ascent of Karjiang?

Chinese alpinists Liu Yang and Song Yuancheng made the first ascent.

They reached the summit after a three-day alpine-style climb of the southwest face and began an extremely difficult descent in snowfall and poor visibility.

What is Karjiang’s first-ascent route called?

The first-ascent route is called Buzzer Beater.

It is approximately 1,300 meters long and was graded AI3, M4, with snow slopes reaching approximately 70 degrees.

How many times has Karjiang been climbed?

The 2025 American Alpine Journal report documents two successful ascents, both completed in 2024.

The first was made by Liu Yang and Song Yuancheng in August. Huang Siyuan and Tong Zhanghao completed the second in September.

Because climbing records from remote parts of Tibet can be slow to appear internationally, future summaries should be checked for more recent expeditions.

Why did Karjiang remain unclimbed for so long?

Karjiang remained unclimbed because of several interconnected challenges:

Steep ice and mixed terrain
Avalanche-prone snow
Hanging seracs
Corniced ridges
Unstable rock near the summit
Unpredictable weather
Difficult acclimatization
Limited rescue possibilities
Restricted access and permit problems
The high cost of a Tibetan expedition

The mountain’s unclimbed status was therefore not caused by one impossible technical section. It resulted from the combined difficulty of reaching, climbing, and safely descending the mountain.

Can ordinary hikers visit Karjiang?

Karjiang is not an ordinary hiking destination.

There is no established public trail to its summit, and the approach crosses remote, high-altitude glacier terrain. Traveling into the area may also require special permissions.

Experienced travelers may be able to see the Karjiang group from authorized routes near Pumo Yumco, depending on current access regulations.

Can Karjiang be climbed without supplemental oxygen?

Both documented 2024 ascents were reported as lightweight alpine-style climbs, and the American Alpine Journal account does not describe the use of supplemental oxygen.

Climbing a 7,221-meter mountain without bottled oxygen requires exceptional acclimatization, judgment, endurance, and high-altitude experience.

What is Karjiang’s easiest route?

Karjiang does not have a conventional easy or normal route.

The southwest face is the only side known to have been successfully climbed, but it remains a major technical route threatened by avalanches, seracs, deep snow, and poor protection.

The second-ascent team’s faster climb does not make the route safe or suitable for less experienced mountaineers.

What is the best season to climb Karjiang?

There is too little climbing history to identify a dependable season.

September provided more stable conditions for the second ascent, while the first ascent succeeded during a narrow August weather window. October has brought cold temperatures and extremely strong winds during earlier expeditions.

Any future attempt would need to evaluate current snow, glacier, wind, and permit conditions rather than relying on a fixed seasonal rule.

Is Karjiang higher than Kula Kangri?

No. Karjiang reaches approximately 7,221 meters, while Kula Kangri is generally reported at approximately 7,538 to 7,554 meters.

Kula Kangri is Karjiang’s parent peak and nearest higher mountain.

Is Karjiang still one of the world’s highest unclimbed mountains?

No. Karjiang lost its unclimbed status when Liu Yang and Song Yuancheng reached the summit on August 13, 2024.

Its successful ascent shifted attention toward other unclimbed 7,000-meter mountains, particularly Gangkhar Puensum, Lapche Kang II, and Apsarasas Kangri I.

What is the difference between Karjiang I and Karjiang II?

Karjiang I generally refers to the 7,221-meter main or south summit.

Karjiang II is less consistent. Older expedition accounts used the name for a roughly 7,216-meter summit climbed by the Japanese in 1986. Some modern classifications instead call that point Karjiang Northwest and identify a separate approximately 7,045-meter summit as Karjiang II or Karjiang Central.

The most accurate approach is to include both the name and elevation whenever referring to a subsidiary Karjiang summit.

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Sources

American Alpine Journal — Karjiang, First Ascent, via Southwest Face — The principal source for the 2024 first ascent, second ascent, route grades, summit coordinates, expedition chronology, bivouacs, weather, and descent.
American Alpine Journal — Karjiang Attempt, Taptol Kangri and Kangmi Kangri First Ascents — First-person record of the 2001 Dutch expedition, avalanche retreat, route reconnaissance, and neighboring first ascents.
American Alpine Journal — Karjiang, Kula Kangri Group — Record of the 1986 Japanese expedition and ascent of the subsidiary 7,216-meter summit.
ExplorersWeb — The Five Highest Unclimbed Mountains: Karjiang I — Historical overview, summit classification, prominence information, nearby mountains, Pumo Yumco, and pre-2024 unclimbed ranking.
ExplorersWeb — Chinese Climbers Make the First Ascent of Karjiang — Contemporary report announcing and summarizing the 2024 first ascent.
Karjiang — Wikipedia — Cross-check for elevation, prominence, coordinates, parent peak, location, and first-ascent date; subsidiary-summit data should be treated cautiously because naming systems differ.
NASA Earth Observatory — Ice on Puma Yumco — Geographic and environmental information about nearby Pumo Yumco.
U.S. Geological Survey — Seismicity of the Himalaya and Vicinity — Authoritative overview of the India–Eurasia collision, Himalayan tectonics, uplift, and regional seismic activity.
PubMed Central — Grazing and Alpine Grasslands of the Qinghai–Tibetan Plateau — Scientific background on the vegetation, ecological functions, and grazing pressures affecting Tibetan alpine grasslands.

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