Khumbu Glacier in the context of "Great Himalayas"

⭐ In the context of the Great Himalayas, the Khumbu Glacier is considered…

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⭐ Core Definition: Khumbu Glacier

The Khumbu Glacier (Nepali: खुम्बु हिमनदी) is located in the Khumbu region of northeastern Nepal between Mount Everest and the Lhotse-Nuptse ridge. With elevations of 4,900 m (16,100 ft) at its terminus to 7,600 m (24,900 ft) at its source, it is the world's highest glacier. The Khumbu Glacier is followed for the final part of the trail to one of the Everest Base Camps. The start of the glacier is in the Western Cwm near Everest. The glacier has a large icefall, the Khumbu Icefall, at the west end of the lower Western Cwm. This icefall is the first major obstacle—and among the more dangerous—on the standard south col route to the Everest summit. It is also the largest glacier in Nepal.

The end of Khumbu Glacier is located at 27°55′55″N 86°48′18″E / 27.932°N 86.805°E / 27.932; 86.805.

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👉 Khumbu Glacier in the context of Great Himalayas

The Great Himalayas (also known as Greater Himalayas, Inner Himalayas, or Himadri) is one of the four parallel sub-ranges of the Himalayas. The core of this part of the Himalayas is composed of granite. It is perennially snowbound. It is the highest in altitude and extends for about 2,300 km (1,400 mi) from northern Pakistan to the Indian state of Arunachal Pradesh, passing through China, India, Nepal, and Bhutan. The sub-range has an average elevation of 6,100 m (20,000 ft) and contains many of the world's tallest peaks, including the eight-thousanders and Mount Everest, the highest peak on Earth. The range is mainly composed of granite rocks with permafrost, and consists of many glaciers, including the Gangotri, Khumbu, and Satopanth Glaciers.

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Khumbu Glacier in the context of Lhotse

Lhotse (Nepali: ल्होत्से, romanized: L'hōtsē [lotse]; Standard Tibetan: ལྷོ་རྩེ, romanized: lho tse, lit.'South Peak' [l̥otse]; Chinese: 洛子峰) is the fourth-highest mountain on Earth, after Mount Everest, K2, and Kangchenjunga. At an elevation of 8,516 metres (27,940 ft) above sea level, the main summit is on the border between the Tibet Autonomous Region of China and the Khumbu region of Nepal.

With Everest to the north and Nuptse to the west, Lhotse forms the apex of the massive horseshoe-shaped arc of the Everest massif. Despite the tremendous vertical relief of its South and Northeast Faces, it is the least prominent of the eight-thousanders due to the great height of the South Col between it and Everest. Lhotse's Western Face, recessed behind the head of the Khumbu Glacier in the Western Cwm, plays an integral part in the standard routes of ascent for both peaks. The name Lhotse, which means "South Peak" in Tibetan, further emphasizes the close relationship between the two.

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Khumbu Glacier in the context of Mahalangur Himal

Mahālangūr Himāl (Nepali: महालङ्गूर हिमाल, Mahālaṅgūra himāla) is a section of the Himalayas in northeast Nepal and south-central Tibet of China extending east from the pass Nangpa La between Rolwaling Himal and Cho Oyu, to the Arun River. It includes Mount Everest, Lhotse, Makalu, and Cho Oyu — four of Earth's six highest peaks. On the Tibetan side it is drained by the Rongbuk and Kangshung Glaciers and on the Nepali side by Barun, Ngojumba and Khumbu Glaciers and others. All are tributaries to the Koshi River via Arun River on the north and east or Dudh Kosi on the south.

Mahalangur Himal can be divided into three subsections:

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Khumbu Glacier in the context of Khumbu Icefall

The Khumbu Icefall is located at the head of the Khumbu Glacier and the foot of the Western Cwm. It lies at an elevation of 5,486 metres (17,999 ft) on the Nepali slopes of Mount Everest, not far above Base Camp and southwest of the summit. The icefall is regarded as one of the most dangerous sections of the South Col route to Everest's summit.

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