The Khumbu Glacier is situated between Mount Everest and the Lhotse-Nuptse ridge in the Khumbu area of northeastern Nepal. It ranges from 4,900 m at its end to 7,600 m at its source in elevation. Between the Lhotse-Nuptse spine and the magnificent Mount Everest, the Khumbu Glacier, which rises to a height of around 24,900 feet, is regarded as the highest glacier in the world. Khumbu Glacier, which forms the final leg of the path and begins at Western Cwm, is crucial for hikers since it connects to Everest Base Camp. Moreover, the Khumbu Icefall, one of the glacier's main features, is well-known to trekkers for serving as a substantial obstacle on their route.
What is Khumbu Glacier?
The shift severely affects the Khumbu Glacier, which is frequently scarred with boulders and other accumulated debris. The coating of flotsam and jetsam mainly protects the ice stream from the effects of rising temperatures on different "smooth" glacial masses because shaking heats more gradually than ice and water. In any event, their benefits are lessened by the existence of puddles on the ice's surface.
Although the pools on the Khumbu are often small, frozen lakes elsewhere in the Himalayas provide a hint of what they may develop into. For example, the icy lake Tsho Rolpa is two miles long and holds roughly 100 million cubic meters of water. It is located just west of Everest.