Engilchek Glacier is a glacier in the Central Tian Shan Mountains of the Issyk-Kul Region in northeastern Kyrgyzstan, with its snout about 50 kilometres east of the village of Engilchek. Its South Engilchek arm ranks as the sixth-longest non-polar glacier in the world and is the largest and fastest-moving glacier in Kyrgyzstan, giving the combined glacier an overall length of about 60.5 kilometres; it descends from the massif of Khan Tengri and Pik Pobedy, and its meltwater feeds the Engilchek River as well as the seasonal glacial Lake Merzbacher, source of frequent glacial lake outburst floods. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
Connections
Caused By
Wikidata P31 formation-type mapped to formative process Glaciation via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Engilchek Glacier
In Discipline
Wikidata P31 formation-type mapped to discipline Glaciology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Engilchek Glacier
In the Other Atlases
- Also in Geography Atlas: China, found in there.
- Also in Geography Atlas: Kazakhstan, found in there.
- Also in Geography Atlas: Kyrgyzstan, found in there.
Sources
Engilchek Glacier (Wikipedia)
Lead sectionQuote, Lead section
Engilchek Glacier (Kyrgyz: Эңилчек, Russian: Энильчек - Enilchek, also Иныльчек - Inylchek) is a glacier in the Central Tian Shan Mountains of Issyk-Kul Region, northeastern Kyrgyzstan.
View the Source Wikidata: Engilchek Glacier
Wikidata Q4534118, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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