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The Khumbu Icefall is located at the head of the
Khumbu Glacier The Khumbu Glacier ( ne, खुम्बु हिमनदी) is located in the Khumbu region of northeastern Nepal between Mount Everest and the Lhotse-Nuptse ridge. With elevations of at its terminus to at its source, it is the world's high ...
and the foot of the
Western Cwm The Western Cwm () is a broad, flat, gently undulating glacial valley basin terminating at the foot of the Lhotse Face of Mount Everest. It was named by George Mallory when he saw it in 1921 as part of the British Reconnaissance Expedition that ...
, which lies at an elevation of on the Nepali slopes of
Mount Everest Mount Everest (; Tibetan: ''Chomolungma'' ; ) is Earth's highest mountain above sea level, located in the Mahalangur Himal sub-range of the Himalayas. The China–Nepal border runs across its summit point. Its elevation (snow heig ...
, not far above
Base Camp Mountaineering or alpinism, is a set of outdoor activities that involves ascending tall mountains. Mountaineering-related activities include traditional outdoor climbing, skiing, and traversing via ferratas. Indoor climbing, sport climbing, an ...
and southwest of the summit. The
icefall An icefall is a portion of certain glaciers characterized by relatively rapid flow and chaotic crevassed surface, caused in part by gravity. The term ''icefall'' is formed by analogy with the word ''waterfall'', which is a similar phenomenon of t ...
is considered one of the most dangerous stages of the
South Col The South Col is a sharp-edged col between Mount Everest and Lhotse, the highest and fourth-highest mountains in the world, respectively. The South Col is typically swept by high winds, leaving it free of significant snow accumulation. Since 195 ...
route to Everest's summit.


Overview

The Khumbu Glacier moves an estimated down the flank of Mt. Everest every day. Ice entering the fall takes approximately 4.3 years to emerge at the base which is 2,000 vertical feet lower and one linear mile away. The speed of ice flow and the precipitous elevation drop, creates a
bergschrund A bergschrund (from the German for ''mountain cleft'') or rimaye (from French; ) is a crevasse that forms where moving glacier ice separates from the stagnant ice or firn above. It is often a serious obstacle for mountaineers, who sometimes ab ...
(ice berg shoulder) characterized at the top by massive transverse blocks that calve off the upper glacier creating gaping
crevasse A crevasse is a deep crack, that forms in a glacier or ice sheet that can be a few inches across to over 40 feet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pie ...
s (hundreds of feet deep and often over 50 feet wide). As these massive initial glacial segments descend the fall, they are slowly twisted and crushed by the churning pressure of glacial flow, generating increasingly torturous crevasse fields in the middle of the fall, and a chaotic maze of smaller blocks toward the bottom of the fall. Due to constant glacial motion, snow bridges concealing crevasses, and overhanging ice blocks (called ''
serac A serac (from Swiss French ''sérac'') is a block or column of glacial ice, often formed by intersecting crevasses on a glacier. Commonly house-sized or larger, they are dangerous to mountaineers, since they may topple with little warning. Even ...
s'') ranging in size from several tons to thousands of tons, can open or collapse with little warning generating extreme danger for climbers. A climber caught in an avalanche or other "movement event" in the icefall can do very little to avoid injury, because the topography of the fall zone prevents fast evasive action. Crossing the Khumbu Icefall is so dangerous that even extensive rope and ladder networks installed by professional guides cannot prevent loss of life. The official Himalayan Database records 44 deaths in the Icefall between 1953 to 2016. No deaths have been recorded between 2017 and 2021. Prudent climbers place emphasis on avalanche and crevasse-fall survival and rescue techniques prior to entering this terrain. Most climbers try to pass through the ice fall before sunrise when it is usually more immobile due to freezing in the nighttime cold. As sunlight warms the area, ice-melt causes friction within the structure to decline, which increases the rate of flow and hence, crevasse opening and ice-block or serac collapse. The most dangerous time to cross the fall is generally mid-to-late afternoon. Experienced, acclimatized climbers can ascend the icefall in a few hours, while inexperienced or non-altitude-acclimatized climbers may take 10–12 hours to complete the passage. "Camp I" on Everest's South Col route is typically slightly beyond the top of the Khumbu Icefall.


2014 avalanche

Around 6:30 am local time on 18 April 2014, 16 Nepalese climbers were killed by an avalanche in the Khumbu Icefall. Only 13 bodies were recovered. Nine others sustained blunt trauma injuries. The climbers were preparing the route through the dangerous icefall for the spring climbing season when the avalanche engulfed them.


References

{{coord, 27, 59, 45, N, 86, 52, 22, E, source:kolossus-frwiki, display=title Glaciers of Nepal Mount Everest