"Hanging Glacier Collapse Triggers Nepal Flash Floods; India Reviews GLOF Preparedness"
GLOF (Glacial Lake Outburst Flood)
sudden catastrophic release of a glacial lake when its moraine or ice dam fails.
LLOF (Landslide Lake Outburst Flood)
flood caused by failure of a river-blocking landslide or debris dam.
The Himalayas are among the world's youngest and most tectonically active mountain systems, formed by the ongoing collision of the Indian and Eurasian tectonic plates. This geological youth produces steep, unstable terrain prone to seismic activity, landslides, and mass-wasting events. The range hosts more than 63,000 glaciers across the Hindu Kush-Himalaya (HKH) region, covering approximately 48,000 sq km in the Himalayan range alone and another 18,000 sq km in the Karakoram. Researchers have mapped over 5,000 glacial lakes across the Himalaya, of which roughly 500 are classified as hazardous or significantly hazardous. As global temperatures rise — at rates considerably faster than the global average in the HKH — glaciers are retreating, permafrost is thawing, and glacial lakes are growing in number and volume, raising the risk of sudden catastrophic releases.
The transboundary character of Himalayan rivers is central to understanding disaster risk. Rivers such as the Bhotekoshi, Koshi, Gandak (Narayani), Karnali, and Trishuli originate in the Tibetan Plateau, cut through Nepal's mid-hills, and enter the Indo-Gangetic Plain, making Bihar, Uttar Pradesh, and other Indian states chronically vulnerable to upstream events. India and Nepal share transboundary river systems governed by the Gandak Treaty (1959) and the Kosi Agreement (1954, revised 1966), but real-time hydrological data sharing and joint early-warning systems remain underdeveloped. India's institutional framework rests on the Disaster Management Act, 2005, which established the National Disaster Management Authority (NDMA), State Disaster Management Authorities (SDMAs), and District Disaster Management Authorities (DDMAs). India is also a signatory to the Sendai Framework for Disaster Risk Reduction 2015–2030, which prioritises proactive risk reduction over reactive relief — a shift that has been slow in practice.
The Bhotekoshi corridor in Nepal's Rasuwa and Nuwakot districts is one of the most hazard-exposed transboundary corridors in the region. It carries the Araniko Highway, the Gyirong (Kerung) Port — a key Nepal-China trade crossing — and the Nepal route of the Kailash Manasarovar Yatra, which crosses into Tibet at the Rasuwagadhi–Gyirong border point. The concentration of trade, pilgrimage, and hydropower infrastructure in this high-gradient valley makes any glacial or flood event here a multi-dimensional crisis.
Himalayan flash floods are driven by several interacting mechanisms. The most severe are Glacial Lake Outburst Floods (GLOFs), which occur when a glacial lake's retaining barrier — made of moraine, ice, or bedrock — fails suddenly. Triggers include moraine collapse, ice or rock avalanches falling into the lake, earthquakes, or rapid snowmelt raising hydrostatic pressure beyond the dam's capacity. The resulting flood wave travels at extreme speed, picking up ice, boulders, and sediment to form a destructive debris flow that can destroy infrastructure many kilometres downstream within minutes. A related but distinct mechanism is an ice-rock avalanche, where a large mass of glacier ice and rock detaches from a high-altitude slope, falls rapidly, and either directly generates a debris flow or temporarily dams a river, creating a barrier lake (also called a landslide dam lake). When this natural dam fails, it releases a secondary flood surge — a Landslide Lake Outburst Flood (LLOF) — that can be as destructive as the initial event. …
Differentiate the causes of landslides in the Himalayan region and Western Ghats.
Explain the mechanism and occurrence of cloudburst in the context of the Indian subcontinent. Discuss two recent examples.
Consider the following pairs:
Glacier — River
1.Bandarpunch — Yamuna
2.Bara Shigri — Chenab
3.Milam — Mandakini
4.Siachen — Nubra
5.Zemu — Manas
Which of the pairs given above are correctly matched?
Consider the following statements regarding glacial hazards in the Indian Himalayan region:
1.ISRO identified 2,431 glacial lakes larger than 10 hectares in Indian Himalayan river basins, of which 676 had expanded notably between 1984 and 2023.
2.The National GLOF Risk Management Programme covers Arunachal Pradesh, Sikkim, Uttarakhand, Himachal Pradesh, Jammu & Kashmir, and Ladakh.
3.A hanging glacier collapse produces a lake-based precursor signal that can be detected by conventional river-gauge early warning systems.
4.A glacial earthquake is seismic energy generated by a glacial collapse itself, not by a tectonic event.
How many of the above statements are correct?
Match the following glacial hazard events with their correct river systems or locations:
1.Chamoli disaster (2021) — (a) Teesta river basin
2.Sikkim glacial lake burst (2023) — (b) Rishiganga/Dhauliganga rivers
3.Nepal flash flood (2026) — (c) Bhote Koshi river corridor
4.Kedarnath tragedy (2013) — (d) Mandakini river valley
Which of the following matchings is correct?
With reference to the National GLOF Risk Management Programme of India, consider the following statements:
1.It covers glacial lakes in Arunachal Pradesh, Sikkim, Uttarakhand, and Himachal Pradesh.
2.It also extends to the Union Territories of Jammu & Kashmir and Ladakh.
3.Its primary mechanism is to install early warning systems on glacial lakes considered vulnerable to breaches.
4.It was initiated following the Kedarnath disaster of 2013.
Which of the statements given above are correct?
Which of the following best describes a 'glacial earthquake' in the context of Himalayan hazard monitoring?
Consider the following statements about the differences between a classic GLOF and a hanging glacier collapse as hazard types:
1.A classic GLOF originates from a glacial lake whose dam fails gradually or suddenly under hydrostatic pressure.
2.A hanging glacier collapse can be monitored in advance using conventional lake-level gauges.
3.Both hazard types produce a debris flow that travels at high speed and carries ice, rock, and sediment.
4.A hanging glacier collapse compresses early-warning time more severely than a classic GLOF because there is no lake-based precursor signal.
Which of the statements given above are correct?
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