Ngozumpa glacier

Ngozumpa glacier is a vast ice field beneath Cho Oyu mountain, covered with layers of rock, sand, and boulders that accumulate on its surface. Its terrain features deep crevasses and unstable zones that make movement across it hazardous.

This glacier formed thousands of years ago during the ice age and has continuously responded to climate shifts over time. Recent decades have brought accelerated retreat, with visible changes in its extent and elevation.

Sherpa communities rely on this glacier's meltwater to sustain their farming and daily water needs in the valleys below. The ice and snow above directly shape how people live and work in these high mountain settlements.

Visitors should arrive with professional guides and proper gear, as the surface is treacherous and filled with hidden dangers. Physical fitness and acclimatization to high altitude are essential before attempting to cross this ice field.

The glacier's melting has created a growing lake that continues to expand year after year, reshaping the landscape. This newly formed water body stands as a visible marker of transformation happening across the ice field.

GPS coordinates: 27.99167,86.69167

Latest update: December 11, 2025 18:06