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Syllabus
GS 1: Important Geophysical phenomena
Context:
Recently, a new study has raised concerns over the increasing number of floods in the Hindu Kush Himalayan region.
More on the News
About Glacial Lake Outburst Floods
Key Highlights from the Study
In the 2000s, glacial floods in the Hindu Kush Himalayas occurred once in 5–10 years. However, in just May and June 2025, ICIMOD recorded three such floods — in Nepal (Limi), Afghanistan (Andorab Valley), and Pakistan (Chitral and Hunza).
This sharp rise is unprecedented and highlights the urgent need to study the causes and manage the risks in the region.
ICIMOD has noted a new trend in recent GLOF events: they are now being triggered by the sudden draining of newly formed ice-dammed supraglacial lakes.
Researchers have stressed the need to strengthen mapping and monitoring of glacial lakes in the Hindu Kush Himalayas.
They recommend updating inventories of potentially dangerous lakes, analysing small and short-lived ice-dammed lakes and including glacier retreat and lake formation processes in hazard assessments.
According to ICIMOD, current monitoring tools are inadequate for the vast and rapidly changing terrain.
It also highlighted the urgent need for better systems to track these changes.
Researchers also warn that by 2100, the region could see a three-fold increase in GLOF risk, making early detection and preparedness even more critical.
About Supraglacial lakes
About Hindukush Mountain
The Hindu Kush is a mountain range in Central and South Asia, primarily spanning:
Length: ~800 km
Orientation: Runs east to west, merging with the Pamir Mountains in the northeast.
Considered the western extension of the Himalayas, though geologically distinct in formation.
Formed as a result of the collision between the Indian Plate and Eurasian Plate.
Lies within the Himalayan-Alpine orogenic belt which is one of the world’s most seismically active zones:
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