Chamar

Chamar

Chamar is a 7,165-meter (23,507-foot) mountain in the remote Sringi Himal of north-central Nepal. Rising east of Manaslu and west of Yangra, it is the highest mountain of a compact Himalayan subrange that receives remarkably little attention compared with its famous neighbors.

The mountain is particularly notable for its extraordinary prominence. Chamar rises approximately 2,061 meters (6,762 feet) above its key col, easily qualifying as an ultra-prominent mountain. Its isolation of almost 25 kilometers further distinguishes it from the many high Himalayan summits that form subsidiary points on larger massifs.

Chamar also has one of the more unusual climbing histories among Nepal’s 7,000-meter peaks. A small New Zealand expedition reached the summit in June 1953, with Maurice Bishop and Nyamgel (Namgyal) Sherpa making the first ascent. Other members reached the summit the following day.

Despite that remarkably early success, the mountain appears never to have received a confirmed second ascent. Japanese-Nepalese climbers came close in 1983 before an avalanche killed one expedition member, while British expeditions in 1994 and 2000 were stopped much lower by logistical problems, dangerous snow, and local opposition to climbing one side of the mountain.

Complicating the story further is Chamar’s elevation. Modern detailed mapping places the principal northern summit at 7,165 meters, while Nepalese government lists have also used 7,187 meters for a separate Chamar entry farther south. Understanding the mountain therefore requires distinguishing modern topography from older and official naming conventions.

⚡ Fast Facts

Fact	Details
Continent	Asia
Country	Nepal
Province	Gandaki Province
District	Gorkha
Mountain Range	The Himalayas
Subrange	Sringi Himal / Shringi Himal
Modern Main Summit	Chamar North
Modern Elevation	7,165 m / 23,507 ft
Nepal Official Chamar Figure	7,187 m / 23,579 ft
South Summit	Approximately 7,161 m / 23,494 ft
Prominence	Approximately 2,061 m / 6,762 ft
Isolation	Approximately 24.99 km / 15.53 mi
Nearest Higher Neighbor (NHN)	Yangra
Key Col	Approximately 5,104 m / 16,745 ft
Coordinates of Modern Main Summit	Approximately 28.553° N, 84.945° E
Peak Classification	Ultra-prominent mountain
First Ascent	June 5, 1953
First Ascenders	Maurice Bishop and Nyamgel Sherpa
Second Summit Party	Graham McCallum, Phil Gardner, and Nima Sherpa
First-Ascent Expedition	New Zealand Himalayan Expedition / Tararua Tramping Club
First-Ascent Route	East or northeast ridge
Supplemental Oxygen	Not used
1983 High Point	Approximately 7,000 m
Confirmed Repeat Ascents	None documented
Climbing Status	Listed by Nepal among expedition peaks
Terrain	Glacier, steep snow, ice, rock, avalanche slopes, and exposed ridges

🏔️ Where Is Chamar?

Chamar rises in Gorkha District of Gandaki Province, north-central Nepal, not far south of the Tibetan frontier.

It forms the highest point of the small but dramatic Sringi Himal, also spelled Shringi, Serang, or Sringi Himal in different sources.

The range lies between major river valleys.

The Shyar Khola and the valleys leading toward Tsum lie to the east, while the Tom Khola and larger river systems toward the Budhi Gandaki and Trisuli watershed define other parts of the surrounding landscape.

Manaslu, at 8,163 meters, rises west of Chamar and is the nearest 8,000-meter mountain.

To the southeast lies the Ganesh Himal, whose highest summit is Yangra at more than 7,400 meters.

Chamar therefore stands between two much better-known Himalayan groups while dominating a distinct range of its own.

📏 How High Is Chamar?

Chamar’s elevation requires some explanation.

Modern detailed topographic mapping places the highest summit at approximately 7,165 meters (23,507 feet).

Peakbagger uses this figure for Chamar’s principal summit at approximately 28.553° N, 84.945° E.

The Himalayan Database similarly distinguishes Chamar North at 7,165 meters from another summit called Chamar at 7,161 meters.

Nepalese government mountaineering publications add another complication.

Some official lists contain:

Chamar — 7,187 meters
Chamar North — 7,165 meters

The official Chamar coordinates correspond closely to the southern part of the massif, where modern mapping identifies a summit closer to 7,161 meters.

This suggests that the 7,187-meter figure is an older survey or mapping value rather than evidence for a separate summit genuinely higher than the 7,165-meter northern peak.

For geographical purposes, 7,165 meters is the strongest modern figure for Chamar’s highest summit.

🗻 Chamar North and Chamar South

The massif contains at least two clearly identifiable major summit points.

The northern summit, usually treated by modern topographic databases as the main Chamar summit, reaches approximately 7,165 meters.

The southern summit lies less than one kilometer away and reaches approximately 7,161 meters.

Peakbagger labels this point Chamar South.

The saddle between the two is around 6,900 meters, giving the southern summit only about 261 meters of independent prominence.

The Himalayan Database likewise separates the peaks, although its terminology calls the southern point simply “Chamar” and the higher summit “Chamar North.”

This naming history explains why older climbing reports can be difficult to compare with modern maps.

The 1953 climbing history is now associated with the 7,165-meter Chamar North summit, which is also the topographically highest point of the massif.

📐 Prominence and Isolation

Chamar has approximately 2,061 meters (6,762 feet) of topographic prominence.

Its key col lies at about 5,104 meters (16,745 feet).

That gives Chamar substantially more prominence than many higher Himalayan mountains.

A peak requires only 1,500 meters of prominence to qualify as an ultra-prominent mountain, so Chamar exceeds the Ultra threshold by more than 500 meters.

Its topographic isolation is approximately 24.99 kilometers (15.53 miles).

The nearest higher terrain lies toward Yangra in the Ganesh Himal.

Chamar’s combination of 7,000-meter elevation, more than two kilometers of prominence, and nearly 25 kilometers of isolation makes it one of the dominant geographical summits of central Nepal.

⛰️ Exceptional Vertical Relief

Chamar’s prominence is only part of its impressive relief.

The mountain rises extremely rapidly from the deep river valleys surrounding the Sringi Himal.

From the Tom Khola–Trisuli drainage region, the summit gains roughly 5,500 vertical meters within about 13 horizontal kilometers.

This is an enormous amount of relief over a short distance.

The result is a landscape in which heavily glaciated 7,000-meter peaks rise almost directly above much lower, deeply incised valleys.

This steepness also helps explain why the Sringi Himal remained so difficult to explore.

Approaches that look short on a map may involve enormous elevation changes, narrow gorges, unstable slopes, river crossings, and complicated glacier systems.

🏔️ The Sringi Himal

The Sringi Himal is one of Nepal’s less familiar Himalayan subranges.

It occupies a relatively small area between the Ganesh Himal and the Manaslu region.

Chamar is its dominant summit.

Unlike the Annapurna, Everest, Manaslu, or Langtang regions, the Sringi Himal never developed into a major international mountaineering or trekking destination.

Its geography contributed to this obscurity.

The range is enclosed by deep valleys, its northern approaches lie near the Tibetan frontier, and its glaciated upper mountains are separated from major population centers by difficult terrain.

As a result, Chamar remained almost unknown to early European mountaineers even while expeditions were exploring nearby Manaslu and the Ganesh Himal.

📝 What Does Chamar Mean?

The origin of the mountain’s name is not well documented in major climbing literature.

Historical sources usually simply use Chamar or Shringi Himal without explaining the etymology.

Because “Chamar” also has unrelated meanings elsewhere in South Asia, assumptions based on modern words or community names should not automatically be applied to the mountain.

The safest approach is therefore to treat Chamar as the established geographical name without assigning it a speculative translation.

The range name also varies considerably in spelling.

Sringi Himal, Shringi Himal, Serang Himal, and similar forms all appear in English-language sources.

🇳🇿 The 1953 New Zealand Expedition

Chamar’s first ascent came during an extraordinary year in Himalayan mountaineering.

A small party from New Zealand traveled to Nepal under the auspices of Wellington’s Tararua Tramping Club.

The New Zealand members included Athol Roberts, Maurice Bishop, Graham McCallum, and Phil Gardner.

Their expedition was very different from the massive national expeditions then attacking mountains such as Everest.

The New Zealanders intended to explore little-known areas of central Nepal rather than concentrate solely on a single famous summit.

They traveled extensively through the Sringi and Ganesh Himal region, investigating mountains and valleys that remained poorly mapped.

Chamar emerged as their greatest climbing objective.

🗺️ Exploring Little-Known Nepal

The expedition took place at a time when large parts of Nepal had only recently become accessible to foreign travelers.

Detailed topographic information was limited.

The New Zealanders explored the eastern headwaters of the Budhi Gandaki and examined several high mountains in the Sringi and Ganesh ranges.

The journey was notable for more than climbing.

Expedition member Phil Gardner collected large numbers of botanical specimens from the region, adding a scientific component to the exploration.

The team also investigated other potential mountain objectives before concentrating on Chamar.

Unlike modern climbers arriving with satellite photographs, GPS tracks, digital elevation models, and decades of expedition reports, the New Zealanders were often discovering the geography while moving through it.

🧊 Choosing the Northeast Ridge

The team identified the east or northeast ridge as the most promising route to Chamar’s summit.

The ridge rises above a complicated glacier basin.

Five camps were established as the climbers pushed progressively higher.

The route involved glacier travel, deep snow, ice, and increasingly exposed ridge climbing.

There was little outside information to guide them because there is no documented earlier attempt on the mountain.

The New Zealanders therefore appear to have been both the first serious climbing expedition to Chamar and the first to succeed.

They climbed without supplemental oxygen.

That was a substantial achievement on a mountain exceeding 7,100 meters, particularly given the limited high-altitude experience and equipment available in 1953.

🏆 First Ascent — June 1953

Maurice Bishop and Nyamgel Sherpa, whose name also appears as Namgyal in historical sources, reached the summit during the first week of June 1953.

The modern Himalayan Database gives the date as June 5, 1953.

Some older printed climbing chronologies instead give June 6, so a one-day discrepancy exists in historical records.

The current Himalayan Database date of June 5 is the clearest modern reference point.

Bishop and Nyamgel had completed the first ascent of Chamar’s highest summit by the northeast ridge.

The achievement came only days after another New Zealander, Edmund Hillary, had made the first ascent of Mount Everest with Tenzing Norgay.

It was an extraordinary moment for New Zealand mountaineering.

🏆 A Second Summit Party

The expedition’s success did not end with Bishop and Nyamgel.

On the following day, Graham McCallum, Phil Gardner, and Nima Sherpa also reached the summit.

This gave the expedition two successful summit parties.

Older climbing chronologies sometimes shift both summit dates forward by one day, listing Bishop and Nyamgel on June 6 and the second party on June 7.

Regardless of that minor dating discrepancy, the sequence is clear: Bishop and Nyamgel reached the top first, followed approximately one day later by McCallum, Gardner, and Nima.

The ascent became one of the highest New Zealand climbing achievements of the early Himalayan era.

🌍 Chamar in the Golden Age of Himalayan Exploration

Chamar’s first ascent occurred during one of the most important years in the history of mountaineering.

Everest was climbed on May 29, 1953.

Chamar followed less than two weeks later.

Nanga Parbat received its first ascent in July.

Nun was climbed in August.

The Himalayas were entering an era in which many of the world’s highest previously unclimbed mountains were being attempted for the first time.

Chamar’s ascent received comparatively little international attention.

That obscurity is understandable given that the first ascent of Everest dominated world news.

Yet reaching a previously unexplored 7,000-meter summit without supplemental oxygen was a major achievement in its own right.

🕰️ Decades Without Another Summit

One might expect Chamar to have accumulated many later ascents.

It did not.

For approximately three decades, there was no major recorded attempt to repeat the New Zealand route.

The reasons included the mountain’s remoteness, lack of established infrastructure, limited international recognition, and the availability of more famous objectives elsewhere in Nepal.

When climbers finally returned during the 1980s, they discovered that the northeast ridge was still a very serious route.

The long interval also meant that glacier and snow conditions had changed substantially from those encountered by the first ascenders.

🇯🇵🇳🇵 The 1983 Attempt

A joint Japanese-Nepalese expedition led by Yoshiharu Miyashiro attempted Chamar in spring 1983.

The team consisted of seven Japanese and three Nepalese climbers.

They chose the east or northeast ridge, effectively trying to repeat the 1953 route.

Three high camps were established.

The expedition prepared a site for Camp IV at approximately 22,300 feet (6,797 meters), although the camp itself was never fully established.

On May 23, four climbers launched a summit attempt.

🧗 High Point Near 7,000 Meters

The summit party consisted of Koichi Akao, Mitsuzu Harada, Mingma Tshering Sherpa, and Dorje Sherpa.

They climbed to approximately 23,000 feet, or around 7,000 meters.

The summit was less than 200 vertical meters higher.

Unfortunately, the ridge ahead remained much longer than expected.

Deep snow made progress slow and exhausting.

The climbers concluded that they could not safely reach the summit and return.

They turned back.

The expedition leader subsequently decided to abandon the attempt.

What happened the next day turned disappointment into tragedy.

Houses in front of Chamar Mountain, Himalaya, Nepal

⚠️ The 1983 Avalanche

On May 24, 1983, the expedition discovered that both tents at Camp II had disappeared.

The site had been hit by an avalanche.

The climbers dug through the snow and found expedition member Koichi Ikari dead.

The avalanche ended any possibility of another attempt.

The tragedy also illustrated one of the central problems on Chamar.

The route is not merely long and technically demanding. Heavy snow and avalanche-prone glacier terrain can make even the lower parts of the mountain exceptionally hazardous.

No confirmed second ascent resulted from the 1983 expedition.

🇬🇧 The 1994 British Expedition

A British expedition led by Rob Brown attempted Chamar in autumn 1994.

The team included ten British climbers, one American, and three climbing Sherpas.

Their goal was to make what they regarded as the first British and second overall ascent.

The expedition encountered problems almost immediately.

Porter difficulties extended the approach by approximately a week.

Once the team reached the mountain, the route proved much longer than expected.

They hoped to climb the northeast ridge but reached only approximately 5,400–5,500 meters.

With insufficient time remaining to mount a serious summit attempt, the expedition withdrew.

🗺️ A Changed Mountain

The 1994 climbers also found conditions different from those described by the New Zealanders four decades earlier.

Glaciers move, retreat, and restructure continuously.

Seracs collapse.

Crevasses open and close.

Snow slopes change according to seasonal accumulation and warming.

A route that was technically possible in 1953 could therefore look dramatically different forty years later.

This is an important characteristic of rarely climbed Himalayan mountains.

On heavily traveled peaks, climbers generate new route information every season.

On Chamar, decades can pass between expeditions, meaning the next party may effectively have to rediscover much of the route.

🇬🇧 British Chamar 2000

Another British-led expedition attempted Chamar in autumn 2000.

The team was led by Tony Barton and included John Allot, Tim Riley, Tom Wiggans, and Swedish climber Peter Berggren.

They held a valid Nepalese permit to attempt the west face.

Their planned Base Camp lay in the Sringi Khola valley.

Before they could establish it, however, the expedition encountered an unexpected obstacle.

A local Buddhist lama objected strongly to their planned ascent of the west face.

🙏 The Sacred West Face

According to the expedition’s published report, the local abbot told the climbers that a deity lived on Chamar’s west face and that the team should not continue farther into the valley.

The expedition’s Sherpa leader and Nepalese liaison officer attempted to negotiate with the lama over several days.

The objection remained.

Rather than force the issue, the climbers abandoned their planned west-face approach.

They then attempted to reach the mountain from another direction.

The eastern side proved no more welcoming.

Snow and avalanche conditions were considered extremely dangerous, similar to those reported by the 1994 British expedition.

The team abandoned its climb at approximately 5,900 meters.

🏔️ Has Chamar Been Climbed Since 1953?

Published climbing records do not identify a confirmed repeat ascent of Chamar’s main 7,165-meter summit.

The 1983 expedition reached close to 7,000 meters but turned back.

The 1994 British team stopped near 5,500 meters.

The 2000 expedition reached approximately 5,900 meters after having to abandon its intended west-face approach.

For this reason, the original 1953 ascent remains extraordinary.

A mountain climbed during the pioneering years of Himalayan exploration has apparently gone more than seven decades without another confirmed ascent.

There are many higher mountains with far more summit traffic.

Chamar remains a striking exception.

🧭 Why Is Chamar Climbed So Rarely?

Several factors combine to keep Chamar exceptionally quiet.

The first is remoteness.

The mountain lies far from Nepal’s best-developed trekking and expedition centers.

Approaches require long journeys through rural Gorkha and the valleys leading toward the Sringi Himal.

The second is technical and objective difficulty.

Chamar’s glaciers are heavily crevassed, its upper ridges are long, and avalanche conditions can become severe.

The third is a lack of modern route information.

Only a handful of expeditions have produced detailed observations since 1953.

Finally, Chamar competes for attention with famous neighbors such as Manaslu and the Ganesh Himal peaks.

For many expedition climbers, easier logistics and more established routes elsewhere are more attractive.

🧊 Glaciers and Terrain

Chamar is a heavily glaciated mountain.

Large glaciers descend from its east, north, and western slopes toward deeply cut valleys.

The summit ridge is surrounded by steep ice and snowfields.

Crevasses and seracs complicate the glacier approaches.

The 1983 attempt demonstrated how deep snow can dramatically slow progress high on the northeast ridge.

Avalanche danger extends far below the summit.

The fatal 1983 accident occurred at Camp II rather than during the final technical climbing.

Later expeditions also considered avalanche conditions serious enough to abandon their attempts.

This combination of glacier instability, deep seasonal snow, and steep relief makes Chamar a mountain where objective hazards can determine success as much as technical climbing ability.

🌦️ Climate and Weather

Chamar lies on the southern side of the main Himalayan divide and receives considerable moisture from the South Asian monsoon.

Summer brings heavy rain to lower valleys and substantial snowfall high on the mountain.

Spring expeditions may encounter deep accumulated winter snow combined with new storms.

Autumn usually offers more stable weather after the monsoon retreats, but early winter winds and heavy post-monsoon snow can still create difficult conditions.

The deep snow that defeated the 1983 summit team illustrates how dramatically the route can change according to seasonal conditions.

Strong winds also affect the exposed upper ridges.

Above 7,000 meters, reduced atmospheric oxygen slows climbers considerably, making long ridge sections especially demanding.

🌿 Flora and Fauna

The valleys below Chamar contain far richer ecosystems than its icy summit might suggest.

Lower elevations in northern Gorkha support Himalayan forests containing species of rhododendron, oak, pine, fir, birch, hemlock, spruce, and juniper.

Higher slopes transition into alpine shrublands and meadows before reaching the permanent snow and glacier zone.

The wider northern Gorkha landscape provides habitat for high-altitude wildlife including Himalayan tahr, blue sheep, goral, musk deer, Himalayan black bears, and the elusive snow leopard.

Smaller alpine mammals include pikas and marmots.

Birdlife includes Himalayan pheasants and large soaring raptors.

Almost none of this biological diversity reaches Chamar’s summit itself, where extreme cold, low oxygen, rock, snow, and ice dominate.

🌸 Alpine Landscapes

The transition between forest and glacier is particularly dramatic in the central Nepal Himalayas.

Rhododendrons can create colorful spring displays at lower elevations.

Higher slopes contain tough grasses, sedges, dwarf shrubs, and seasonal wildflowers capable of surviving long winters.

Above the alpine meadows, exposed rock and moraine increasingly dominate.

Eventually, permanent snow and ice replace vegetation entirely.

Because Chamar rises so sharply above nearby valleys, several ecological zones can occur within a relatively small horizontal distance.

This steep environmental gradient is one of the defining characteristics of the Sringi Himal landscape.

🥾 The Tsum Valley Region

The eastern approaches to the Sringi Himal are associated with the broader Tsum Valley region.

Tsum is a culturally distinctive high Himalayan valley connected historically with Tibetan Buddhism.

Villages, monasteries, mani walls, chortens, prayer flags, and agricultural terraces characterize the inhabited landscape below the high peaks.

Modern government mountaineering information lists the caravan approach toward Chamar through Arughat, Jagat, and the Tsum Valley.

This does not turn Chamar into an ordinary trekking mountain.

The established trekking routes remain far below the summit, and reaching a climbing Base Camp requires substantially more specialized expedition logistics.

🙏 Mountains and Local Beliefs

The experience of the 2000 British expedition demonstrates that high mountains may have cultural meanings very different from those assumed by visiting climbers.

The team possessed official government permission to climb Chamar’s west face.

Local religious leaders nevertheless opposed the expedition because of beliefs associated with that side of the mountain.

The team ultimately respected the objection and changed its plans.

It would be inappropriate to conclude from one incident that every community around Chamar shares exactly the same beliefs.

The episode does, however, illustrate an important feature of Himalayan mountaineering: a government climbing permit does not necessarily erase local cultural and spiritual relationships with a mountain.

🪨 Geology

Chamar formed through the same enormous tectonic collision responsible for the Himalayas.

The Indian Plate continues to move northward into the Eurasian Plate.

This collision has compressed, folded, faulted, and uplifted vast masses of crust to produce the Himalayan mountain chain.

Central Nepal contains complex sequences of metamorphic and sedimentary rocks affected by major Himalayan thrust systems.

Uplift alone did not create Chamar’s modern form.

Glaciers and rivers have carved deeply into the rising terrain.

The extraordinary relief around the Sringi Himal reflects the combined effects of tectonic uplift and intense erosion.

Earthquakes, landslides, glacier movement, frost weathering, and river incision continue reshaping the landscape today.

🏔️ Nearby Mountains

Yangra rises southeast of Chamar and reaches approximately 7,429 meters. It is the nearest higher mountain and the highest summit of the Ganesh Himal.

Manaslu lies to the west and reaches 8,163 meters, making it the nearest 8,000-meter peak.

Himal Chuli rises near Manaslu to approximately 7,893 meters and is another dominant summit of the Mansiri Himal.

Ganesh II and Pabil are among the other major 7,000-meter mountains to the southeast.

The position of Chamar between the Mansiri and Ganesh groups helps explain why it has been overshadowed despite its own exceptional prominence.

🧭 Can Chamar Be Climbed Today?

Nepal continues to list Chamar among its expedition mountains.

Government mountaineering publications distinguish both Chamar and Chamar North, although their published elevations and naming do not align perfectly with modern topographic mapping.

The official approach is generally described through Arughat, Jagat, and Tsum Valley toward Base Camp.

A permit alone does not guarantee that an expedition will be straightforward.

Modern climbers would need to consider local access arrangements, cultural concerns, glacier changes, avalanche conditions, and the scarcity of recent route information.

There is no heavily used normal route with fixed infrastructure comparable with commercial Himalayan peaks.

Any attempt on Chamar should be considered a serious exploratory high-altitude expedition.

⭐ Why Chamar Is Remarkable

Chamar deserves far more attention than it receives.

At approximately 7,165 meters, it is not among Nepal’s very highest mountains, yet its 2,061 meters of prominence make it one of the country’s most topographically independent 7,000-meter peaks.

It rises more than five vertical kilometers above nearby valleys.

Its first ascent came in 1953, during the same extraordinary season as the first ascent of Everest.

A small New Zealand team entered a poorly mapped region, identified a route, established five camps, and put two parties on the summit without supplemental oxygen.

Then the mountain almost disappeared from mountaineering history.

Thirty years later, a Japanese-Nepalese team came close but was stopped by deep snow and a fatal avalanche.

British expeditions in 1994 and 2000 were defeated much lower.

Modern mapping subsequently complicated even the mountain’s basic identity by revealing differences between the official Chamar, Chamar North, and Chamar South designations.

The result is one of the Himalayas’ most intriguing forgotten giants — an ultra-prominent 7,000-meter mountain whose summit may have been visited only during a few days in June 1953.

❓ Frequently Asked Questions

How high is Chamar?

Modern detailed mapping places Chamar’s highest northern summit at approximately 7,165 meters (23,507 feet). Nepalese government publications have also listed a separate “Chamar” at 7,187 meters.

Why do some sources say Chamar is 7,187 meters?

Nepal’s official peak lists historically assigned 7,187 meters to Chamar while separately listing Chamar North at 7,165 meters. Modern topographic data indicate that the northern 7,165-meter summit is actually the highest point and that the southern summit is closer to 7,161 meters.

Where is Chamar?

Chamar is located in Gorkha District, Gandaki Province, Nepal, in the Sringi Himal between the Manaslu and Ganesh Himal regions.

Is Chamar the highest mountain in the Sringi Himal?

Yes. Chamar is the highest summit of the Sringi Himal.

Who first climbed Chamar?

Maurice Bishop and Nyamgel Sherpa made the first ascent.

When was Chamar first climbed?

The Himalayan Database records the first ascent on June 5, 1953. Some older climbing chronologies give June 6.

Who reached the summit after the first ascenders?

Graham McCallum, Phil Gardner, and Nima Sherpa reached the summit approximately one day after Bishop and Nyamgel.

What route did the first climbers use?

They climbed the east or northeast ridge and established five camps.

Did the first ascenders use supplemental oxygen?

No. The 1953 New Zealand expedition climbed Chamar without bottled oxygen.

How prominent is Chamar?

Chamar has approximately 2,061 meters (6,762 feet) of topographic prominence.

Is Chamar an ultra-prominent mountain?

Yes. Its prominence comfortably exceeds the 1,500-meter threshold used to define an Ultra.

What is Chamar’s nearest higher neighbor?

The nearest higher mountain is Yangra in the Ganesh Himal.

Was Chamar nearly climbed again in 1983?

Yes. A Japanese-Nepalese summit party reached approximately 7,000 meters before deep snow and the length of the remaining ridge forced a retreat.

What happened during the 1983 expedition?

An avalanche struck Camp II after the summit attempt and killed Japanese climber Koichi Ikari.

Why did the 2000 expedition abandon the west face?

A local Buddhist lama objected to climbing the west face because of spiritual beliefs associated with the mountain. The expedition changed its approach but was later stopped by dangerous avalanche conditions.

Has Chamar been climbed more than once?

No confirmed second ascent appears in the major published climbing histories. The 1953 ascent remains the only documented successful expedition to the main summit.

Can Chamar still be climbed?

Yes. Nepal lists Chamar among its expedition mountains, but climbing it requires appropriate permits, local access arrangements, extensive expedition experience, and the ability to operate in remote avalanche-prone terrain.

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