Kunlun Mountains
Major mountain chain along the northern edge of the Tibetan Plateau in western China, notable for high peaks, complex geology, volcanic features, and deep cultural significance in Chinese history and mythology.
Overview
The Kunlun Mountains are a long, complex mountain system that runs roughly east–west along the northern margin of the Tibetan Plateau. Often cited as one of the major ranges of interior Asia, the Kunlun form an important topographic boundary in western China and link with neighboring systems to the west and north. Their exact limits and subdivisions are treated differently by geographers and cartographers, so descriptions of area and length can vary.
Image gallery
5 ImagesGeography and landscape
Stretching across high plateaus, deserts and alpine basins, the Kunlun include glaciers, high passes and long ridgelines. Several rivers have their headwaters in or near the range, and its slopes feed tributaries that flow into larger interior drainage systems. The terrain ranges from ice- and snow-covered summits to arid foothills and salt flats where elevation drops toward adjacent basins.
Geology, peaks and volcanism
Geologically the Kunlun are the product of continental collision and uplift associated with the India–Eurasia convergence; complex faulting and folding create varied rock types and elevations. The range contains numerous high summits; some sources name a prominent peak sometimes referred to in English as the "Kunlun Goddess" with an elevation cited in the 7,000-metre class, though peak names and exact heights are treated differently on different maps.
The range also exhibits volcanic features in places. Certain volcanic summits in the broader Kunlun region reach elevations in the mid‑5,000‑metre range, and some reports note activity in the 20th century. Precise identification and dating of volcanic events vary among geologic studies, so accounts commonly qualify specific eruption dates and heights.
Cultural significance and history
Beyond physical geography, the Kunlun occupy an important place in Chinese literary and religious traditions. In classical myth, Kunlun is portrayed as a sacred mountain or a paradisiacal domain inhabited by deities and immortals. Historical travelers, trade routes and frontier communities have long adapted to the region's challenging environment, leaving traces of human use and seasonal pastoralism.
Ecology, uses and notable facts
- High‑altitude ecosystems include alpine meadows, cold deserts and glacial environments that support specialized flora and fauna.
- The range influences regional climate patterns and water supply for downstream landscapes.
- Mapping and naming conventions differ; for more detailed geographic or scientific data consult regional studies and maps.
For general geographic context see a regional description of the Kunlun mountain system, and for accounts addressing volcanic features consult sources that discuss specific volcanic summits in the area.
Mountains
The mountain ranges of Kunlun Shan have over 200 peaks of more than 6000 m in height. The mountains include:
- Liushi Shan - Kunlun Goddess (7167 m, ⊙35.31414380.9168957167)
- Ulugh Muztagh (6973 m, ⊙36.412587.38416666676973).
- Bukadabang Feng (6860 m, ⊙36.02416790.8658336860).
- Yurung Shan I (6778 m, ⊙35.37168481.1786926778)
- Yurung Shan II (6767 m, ⊙35.36143981.1059816767)
- Kotaklik Shan (6580 m, ⊙35.99394181.5940936580)
- Yuzhu Shan (6178 m, ⊙35.652594.2508336178)
- Malan (6056 m)
- Tekiliki Day (5466 m)
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Map with all coordinates of the section Mountains: OSM
Earth History
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This article or section needs revision. More details should be given on the discussion page. Please help improve it, and then remove this tag.
The Kunlun Mountains were formed by the collision of the Indian subcontinent plate with the Eurasian plate, closing the primordial ocean known as the Tethys.
The mountains, rich in mineral resources, are largely a high mountain desert.
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Author
AlegsaOnline.com Kunlun Mountains Leandro Alegsa
URL: https://en.alegsaonline.com/art/54633

