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  2. Tectonics of the Tian Shan - Wikipedia

    en.wikipedia.org/wiki/Tectonics_of_the_Tian_Shan

    West Tian Shan mountains. The Tian Shan is a mountain range in central Asia that extends through western China, Kazakhstan, and Kyrgyzstan. [1] The Tian Shan is 2,800 kilometres (1,700 mi) long, and up to 7,400 metres (24,300 ft) high. Throughout the Tian Shan there are several intermontane basins separated by high ranges. [1]

  3. Geology of China - Wikipedia

    en.wikipedia.org/wiki/Geology_of_China

    The Tian Shan are a mountain range north of the Tibetan Plateau and the Taklamakan Desert. Uplift of these mountains began 24 million years ago. It was a direct response to the continued extension of the Indian collision zone. The mountain range is still uplifting today along with the Himalaya. [9] [10]

  4. Tian Shan - Wikipedia

    en.wikipedia.org/wiki/Tian_Shan

    Altogether, the glacial Tian Shan glaciation occupied an area of approximately 118,000 square kilometers. The glacier snowline was about 1200m lower during the last ice age than it is today. This would result in a depression of the average annual temperature of 7.2 to 8.4 °C for the Last Glacial Maximum compared with today, assuming a ...

  5. Geology of Kyrgyzstan - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Kyrgyzstan

    The Paleozoic rocks in the Tien Shan mountains are the remnants of accreted island arcs, mainly from the Ordovician onward. During the Vendian , the Northern Turkestan domain was part of the Kipchak island arc system between the East European and Siberian continent, separated by the Terksey back-arc basin which had originated as a rift basin.

  6. Glacier morphology - Wikipedia

    en.wikipedia.org/wiki/Glacier_morphology

    Franz Josef Glacier in New Zealand Features of a glacial landscape. Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. [1] The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. [2]

  7. Mountains of Central Asia - Wikipedia

    en.wikipedia.org/wiki/Mountains_of_Central_Asia

    Central Asia physical map. The Mountains of Central Asia are a biodiversity hot spot designated by Conservation International which covers several montane and alpine ecoregions of Central Asia, including those of the Pamir and Tian Shan ranges, and extending across portions of Afghanistan, China, Kazakhstan, Kyrgyzstan, Tajikistan, Uzbekistan and the Karakoram range in China, Pakistan and India.

  8. Tian Shan foothill arid steppe - Wikipedia

    en.wikipedia.org/wiki/Tian_Shan_foothill_arid_steppe

    The Tian Shan foothill arid steppe ecoregion (WWF ID: PA0818) covers the northern and western approaches to the Tian Shan mountains, centered on Lake Issyk-Kul in Kyrgyzstan. This region receives more moisture from Central Asia, thereby supporting more vegetation and diversity of plant and animal species than the deserts to the south.

  9. Tian Shan montane steppe and meadows - Wikipedia

    en.wikipedia.org/wiki/Tian_Shan_montane_steppe...

    The Tian Shan montane steppe and meadows ecoregion (WWF ID: PA1019) covers a 2,000 km long stretch of grasslands of the isolated Tian Shan mountains of Central Asia. It is characterized by high-altitude flat and rolling grasslands. [1] [2]