Category: History and Culture

Welcome to our blog, where we explore the tragic story of “what is Manaslu avalanche?”, a compelling account of survival, disaster, and determination that affects the world of mountaineering. Join us as we explore the details of the fatal day on Mount Manaslu and its significant impact on climbers and the global climbing community.

Understanding Mount Manaslu:

Mount Manaslu is the eighth-highest peak in the world, with an elevation of 8,163 meters (26,781 feet). It is in the stunning landscapes of the Nepalese Himalayas. The mountain’s beauty and terrain have always attracted adventurers and mountaineers who want to beat one of the highest peaks in the world. 

Quick Overview of What is Manaslu Avalanche

Before getting in-depth into the what is Manaslu avalanche, let’s get familiar with what is avalanche first.

So, what comes to your mind when someone talks about an avalanche?

An avalanche is a condition where a mass of snow, ice, or rocks falls rapidly down a mountainside. Have you ever wondered why it falls?

Let’s get this clear. Every time snowfall occurs, there is a layering of snow. The new snow always takes time to blend and adjust with firmly attached old snow. If something disturbs it, the structure becomes unstable and can initiate an avalanche.

Many avalanches begin after the storm. Snowfall of more than 50 cm within 24 hours is unstable. The fact that old snow needs time to blend with the new snow. In such cases, if the snow is affected due to some factors, it can be devastating and lead to an avalanche.

Types of Avalanche

1. Slab Avalanche:

• Slab avalanches are hazardous and have the potential to cause notable destruction. They occur when a cohesive layer of snow separates from the underlying snowpack and proceeds downhill as a unified mass. This cohesive layer, referred to as the slab, can be set off by different factors:
  • There is a rapid accumulation of snow due to precipitation.
  • Wind deposition can create thick slabs on leeward slopes.
  • Mechanical stress is like the weight of a skier or snowboarder.
• Slab avalanches can pose significant threats to anything in their path as they often occur on steep slopes and can travel long distances.

2.  Point Release Avalanche:

• Loose snow avalanches, also known as sluffs, are called point-release avalanches. These avalanches occur when a smaller amount of snow is released compared to slab avalanches. Instead of a stable slab splitting off, separate loose snow particles or small snow pockets detach from the surface and flow downhill.
  • These avalanches typically occur on steep slopes, often triggered by factors such as:
    • Warming temperatures can destabilize the snowpack and cause surface layers to become lubricated.
    • A human or animal activity like skiing loosens the snow.
    • Rainfall can saturate the snowpack and lower its cohesion.
• Although point-release avalanches typically involve smaller amounts of snow compared to slab avalanches, they still present dangers to individuals traveling in the backcountry and have the potential to bear more snow and trash as they move downward.

What Kind of Avalanche is Dangerous?

Most of the avalanches across the world occur due to humans and animals. Only after that the mountains and terrains are responsible.

Almost all Avalanches occur at a slope of 30 to 45 degrees. The most dangerous one is from a 37-degree slope. They tend to fall quickly and leave deadly traces.

Due to the immediate change in weather resulting from global warming, there is a rapid change in snow patterns. This unusual change results in the factors causing an avalanche.

Why is an Avalanche a Risk?

Trek usually occurs below 5800 meters, and the snow line hits from 4000 meters. Hence, it has the risk factor of an avalanche while trekking or mountaineering at a high altitude. Victims have a 15-minute golden period for survival after an avalanche. However, there is no such technology in Nepal to prevent snow victims within 15 minutes of the current situation.

Factors Causing Avalanches:

1. Human/ Animals
2. Weather
3. Snowpack(old snow)
4. Terrain

Human/Animals:

• Human activity, such as skiing, snowboarding, or hiking, can sometimes trigger avalanches, especially when venturing into avalanche-prone terrain without proper knowledge or precautions.
• Herds of grazing animals or humans traveling with animals can disturb snowpack stability and potentially trigger avalanches, particularly in areas with heavy snow accumulation.

Weather:

• Rapid temperature changes, such as sudden warming after a cold spell, can weaken the snowpack and increase the likelihood of avalanches by promoting snowpack settlement or the formation of weak layers within the snowpack.
• The formation of avalanches is affected by weather. When there is heavy snowfall, particularly in combination with strong winds, the amount of snow on slopes can quickly become excessive, resulting in unstable conditions.

Snowpack (Old Snow):

• Older layers of snow buried beneath newer snow can become weak and unstable over time, especially if subjected to additional snowfall or temperature fluctuations, creating potential weak points where avalanches can release.
• Avalanche risk depends on the snowpack’s composition and structure of weak layers or faceted snow crystals.

Terrain:

• Terrain characteristics, including slope angle, aspect, and vegetation cover, play a crucial role in avalanche formation.
• The orientation of a slope relative to the sun can affect the stability of its snowpack. South-facing slopes are usually more susceptible to instability due to solar radiation-induced melting.
• Steep slopes, typically with angles between 30 and 45 degrees, are most prone to avalanches due to the gravitational force acting on the snowpack.

Safety Considerations for Both Victim And Trek Guide During Avalanche

Why is Manaslu Prone to Avalanche?

• High Altitude: Towering at the peak where the air is thin and weather changes quickly make an avalanche more likely.    
• Steep Slopes: The mountain’s steep sides mean snow and ice can build up and then slide down as avalanches, especially after snowfall or temperature changes.
• Glacial Motion: Manaslu has glaciers that constantly shift and move, which can destabilize snow and ice, leading to avalanches.
• Serac Formation: Large ice blocks called seracs can collapse, triggering avalanches.
• Monsoon Season: Heavy rainfall and snowfall during the monsoon season can create unsafe snowpacks, increasing avalanche risk.
• Wind Effects: Strong winds on Mount Manaslu can transport snow from one area to another, creating unstable snow deposits prone to triggering avalanches.
• Temperature Changes: Rapid temperature changes, especially during daytime and nighttime or between seasons, can weaken the snowpack and increase the likelihood of avalanches.
• Snowpack Layers: Different layers of snow can form on the mountain over time, and if these layers don’t bond well, they can create weak points in the snowpack, leading to avalanches.
• Human Action: Climbers and mountaineers traversing the slopes of Mount Manaslu can inadvertently trigger avalanches through their movements if they disturb unstable snow formations or seracs.
• Recorded Avalanche Paths: Previous avalanche paths on the mountain may be prone to recurring avalanches as the terrain and conditions remain favorable for snow to slide down again.

Conclusion

After considering different factors, we can answer“ what is Manaslu avalanche” as we have determined that Mount Manaslu’s vulnerability to avalanches is affected by several factors. By following proper advice and trusting the right travel planner, individuals can safely experience the beauty of Mount Manaslu and create lasting memories. Respecting the mountain’s natural processes and implementing safety measures can help minimize the risk of avalanches while appreciating the breathtaking beauty of this glorious peak in the Himalayas.

Frequently Asked Questions (FAQs)

Introduction to Mt. Manaslu: How was Manaslu Formed

Mt. Manaslu holds a significant place in the hearts of mountaineers and adventure enthusiasts and concern about how was Manaslu formed. Mt. Manaslu, also known as the ‘Mountain of the Spirit,’ is located in the Gorkha District of Nepal. It has an impressive height of 8,163 meters (26,781 feet) and is considered a sacred peak by the locals, who refer to it as ‘Kutang’ or ‘the holy peak.’ Its history is intertwined with mythologies, treacherous expeditions, and vibrant cultural customs. The local community deeply reveres this mountain and attributes religious significance to it. The ambience of mystique surrounding Mt. Manaslu captivates anyone who ventures into its enigmatic depths, thanks to the captivating local narratives.

Exploration and Early Attempts in Mt. Manaslu:

The exploration of Mt. Manaslu started in the early 20th century when mountaineers were drawn to the challenge of climbing the world’s 8th highest peak. The mountain presented difficulties for examination due to its remote location and challenging terrain. The first expedition to climb Manaslu occurred in 1952, led by Toshio Imanishi and a team of Japanese climbers.Despite their best efforts, the team had to retreat due to the difficult weather conditions and dangerous avalanches.

However, they made a second attempt on May 9, 1956, led by Yuko Maki, and successfully reached the summit of Mount Manaslu. This achievement, along with the participation of Gyalzen Norbu and other team members, was highly regarded and celebrated in the history of Himalayan mountaineering. After the successful climb, several expeditions from different countries made attempts to climb Manaslu, but only a small number were able to reach the summit. Despite the numerous challenges they faced, Mount Manaslu continues to attract climbers from around the globe.

Significance Location: 

Mt. Manaslu’s location holds profound significance both geographically and culturally. Positioned as the eighth-highest peak in the Himalayas, its towering presence not only offers breathtaking vistas but also serves as a vital navigational landmark for travelers and mountaineers. Culturally, it is revered as the “Mountain of the Spirit,” embodying sacredness and spirituality for local communities who pilgrimage to its base seeking blessings. Surrounding the mountain are diverse ethnic groups, enriching the region with vibrant traditions and customs.

Additionally, its remote location and challenging terrain attract researchers and adventure seekers, offering opportunities for exploration and scientific study. Thus, Mt. Manaslu’s location stands as a nexus of geographical marvels, cultural heritage, and spiritual sanctity, inviting all who encounter it to partake in its awe-inspiring presence.

Geological Background:

Mt. Manaslu is situated in the heart of the Himalayas, a region known for its complex geological history. The formation of this majestic peak is deeply rooted in tectonic movements that have shaped the landscape over millions of years. The collision of the Indian Plate with the Eurasian Plate has played a crucial role in the upliftment of the Himalayan range, including Manaslu. The intense pressure exerted by these tectonic forces has led to the buckling and folding of the Earth’s crust, giving rise to towering peaks like Manaslu. Additionally, the region’s geological composition, characterized by layers of sedimentary, metamorphic, and igneous rocks, contributes to the unique features observed in Manaslu and its surrounding landscape.

Geological Features:

Mt. Manaslu exhibits a diverse range of geological features that showcase the dynamic processes at work in the Himalayan region. The mountain is predominantly composed of granite, gneiss, and schist, which were formed through the cooling and solidification of magma deep within the Earth’s crust. Over time, the relentless forces of erosion, including glaciers, rivers, and weathering, have sculpted the rugged terrain of Manaslu. Glacial valleys, cirques, and moraines dot the landscape, evidence of the powerful influence of ice on shaping the region. Additionally, the presence of fault lines and fractures in the rock formations indicates ongoing tectonic activity in the area, contributing to the seismicity of the Himalayas.

Formation:

The formation of Mt. Manaslu can be attributed to a combination of geological processes that have unfolded over millions of years. The initial stages of its formation can be traced back to the collision of the Indian and Eurasian Plates around 50 million years ago. This collision resulted in the upliftment of vast sedimentary deposits, forming a massive mountain range that would later evolve into the Himalayas. 

Subsequent tectonic activity, including crustal thickening and uplift, further sculpted the landscape, giving rise to individual peaks like Manaslu. The ongoing convergence of the Indian Plate continues to exert pressure on the region, contributing to the gradual upliftment and deformation of the Himalayas. Today, Mt. Manaslu stands as a testament to the geological forces that have shaped the Earth’s surface, serving as a symbol of both natural beauty and geological complexity.

Conclusion:

Mt. Manaslu is appealing to mountaineers, adventure seekers, and nature enthusiasts, and one of the concerns is how was Manaslu formed. Despite the challenges it presents to climbers, being the 8th highest peak in the world, it still attracts climbers from around the globe. The Manaslu region is inhabited by diverse ethnic groups, each with their own unique culture and traditions. Visitors can expect a warm welcome from the friendly and polite locals of the Manaslu region. In the Himalayas, Mt. Manaslu and its surrounding area are known for their stunning natural beauty, cultural heritage, and opportunities for mountaineering. It continues to attract adventurous travelers looking for a unique and rewarding experience.

Frequently Asked Questions (FAQs)