Panmah Glacier, Glacier in Gilgit-Baltistan, Pakistan
Panmah Glacier is an extensive ice formation in the Karakoram mountain range that stretches across a wide valley with a rough, fissured surface. The landscape features steep snow-covered slopes, narrow valleys, and fields of rocky debris scattered throughout the entire region.
This glacier formed during earlier ice ages as part of the vast Karakoram glacial systems that developed over long periods. Its ice mass has changed over time like other mountain glaciers, responding to shifts in climate conditions.
Local communities depend on the meltwater from this glacier for their water supply and have developed strong connections to this landscape over generations. The way people use the water has shaped their daily routines and settlements in the region.
Reaching this glacier requires mountaineering experience and specialized equipment since it sits in a remote location at high elevation. The rough terrain with deep crevasses and steep slopes means you need to travel with experienced guides and proper safety gear.
The surface is scattered with rock debris, giving it a speckled appearance that sets it apart from pure white glaciers. This mix of ice and stones forms because of constant rockfall and weathering in this active high mountain region.
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