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Kangshung Glacier

glacier in Tibet

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Record originEnglish Wikipedia
Text licenseCC BY-SA 4.0
Source revisionJul 3, 2026
Entity authorityQ1723747 ↗
Source-derived summary

The Kangshung Glacier (Chinese: 卓穷冰川) is one of the three main glaciers of Mount Everest, and is in the Tibet region Himalayas, within the Tibet Autonomous Region of China. The other two are the Khumbu Glacier and Rongbuk Glacier.

Geography

The Kangshung Glacier's accumulation areas lie on the three main faces of Everest. The Kangshung Glacier is located on the eastern side of the world's highest mountain in the government district of Shigatse in the Tibet Autonomous Region of the People's Republic of China.

The common eastern face of Everest and Lhotse is called the Kangshung Face. Here, the Kangshung Glacier is fed and then becomes the Kama Chu river to flow through the Kama valley towards the east. South of the glacier and east of Lhotse lie the Pethangtse (6738 m), and the massif of the Makalu (8463 m) with its neighbouring peaks of Makalu II (7678 m − also called Kangshungtse) and Chomo Lonzo (7818 m), whose imposing north face hides the view of the main Makalu summit. The border between Nepal and China runs over this summit.

Access

The east side of Mount Everest is the least accessible and developed side of the mountain. While the base camp on the Rongbuk Glacier can be accessed by jeep and the south side of Everest can be reached after a multi-day hike using fortified lodges for overnight stays, the Kangshung Glacier can only be reached following an approach march of several days from Kharta, including crossing via the Shao La or Langma La passes into the Kama valley.

Editorial summary

This brief starts where responsible research should: with the source description of “Kangshung Glacier” as glacier in Tibet. Everything that follows is an evidence route, not borrowed authority.

Editorial reviewA practical starting point whose main value is the path it opens into stronger specialist and primary sources. The current 259-word lead offers orientation but no explicit four-digit date, so chronology should not be assumed. The selected authority fields contribute no independent date. The account is most persuasive where Kangshung, Glacier and glacier can be independently traced.
Editorial analysis

Why this record matters

The subject matters to the general reference register because the source frames it as glacier in Tibet. Its deeper value depends on whether names, dates, institutions and citations support that framing.

Evidence profile

Vocabulary and entity names are the principal evidence signals here, because they determine the precision of every later search. The source revision retrieved here is dated Jul 3, 2026. The linked authority identifier is Q1723747. Authority coordinates are 27.985, 87.050. 2 of 2 selected statements include explicit references; 0 carry qualifiers and 0 use preferred rank.

Critical limits

Overview language is designed for orientation and should not be treated as a substitute for the evidence cited beneath it. The lead is largely declarative, so disagreement and counter-evidence require a deliberate search beyond the opening account. Authority statements aid reconciliation but still require their own references, qualifiers and ranks to be checked.

How to read it

Use the entry as an orientation point, then follow its citations and revision history. Names, dates and institutional relationships should be checked against the original record.

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Source & attribution

This entry incorporates text from “Kangshung Glacier” on English Wikipedia. Contributors are listed in the page history. Text is available under the Creative Commons Attribution-ShareAlike 4.0 License. Selected authority identifiers and statements are retrieved from Wikidata under CC0; their references and qualifiers remain part of the verification path.