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. The Karakoram range is also famously known for Karakoram Anomaly that relates to the anomalous growth of glaciers in the central Karakoram that is in contrast with melting glaciers in other mountainous ranges of Himalayas and other parts of the world due to the effects of climate change.
Katon-Karagay National Park is the largest national park in Kazakhstan, located on the eastern edge of the country, in the Southern Altai Mountains. The park fills the west side of the "X" where the borders of Kazakhstan, Russia, China, and Mongolia meet. The highest peak in Siberia, is on the Russian border in the Katun Range. The park is in Katonkaragay District of East Kazakhstan Region, 1,000 kilometres (620 mi) southeast of the capital city of Astana.
Zhongar-Alatau National Park, also Jungar Alatau, or Dzungurian Alatau, was created in 2010 to protect the unique ecology of the Dzungarian Alatau, an isolated, glaciated mountain range in Kazakhstan, on the southeastern border with China. One stated reason for creating the park is to protect forests of wild fruit trees, including apricots, barberry, cherries, and currants. Approximately 1% of the land area of the park is forested with Sievers Apple trees, which are the progenitors of all cultured apple varieties in the world. The park is 300 km long (west-to-east), and spreads across Aksu District, Sarkand District and Alakol District of Almaty Region, 300 km northeast of the regional city of Almaty.
The Altai montane forest and forest steppe ecoregion covers patches of the subalpine forest belt on the Altai Mountains, crossing the border region where Russia, Kazakhstan, Mongolia and China meet. The region has high biodiversity, as it is located in transition zones between different ecoregions, altitudes, and climate zones. It is in the Palearctic realm, with a Cold semi-arid climate. It covers 35,199,998 km2 (13,590,795 sq mi).
The Altai alpine meadow and tundra ecoregion is a terrestrial ecoregion covering the higher elevation of the Altai Mountains at the center of the "X" formed by the borders separating Russia, Kazakhstan, China, and Mongolia. The mountain peaks are the farthest north in Central Asia, separating the plains of Siberia to the north from the hot, dry deserts to the south. Altitudes above 2,400 meters display characteristics of tundra, with patches of alpine meadows and some trees immediately below the treeline. The ecoregion is in the montane grasslands and shrublands biome, and the Palearctic realm, with a humid continental climate. It covers an area of 90,132 square kilometres (34,800 sq mi).
The Tian Shan montane conifer forests ecoregion covers the "forest belt" of the Tian Shan mountains - generally the north-facing slopes that get enough moisture, and are warm enough, for trees to grow. This conifer belt is found mostly between 1,500 and 2,700 meters.
The Tian Shan montane steppe and meadows ecoregion 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.
The Tian Shan foothill arid steppe ecoregion 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.
The Central Tibetan Plateau alpine steppe ecoregion covers the high alpine plateau that stretches over 1,600 kilometres (1,000 mi) across the Tibetan Plateau to Qinghai Lake in China. Because of the high altitude—much it over 5,000 metres (16,000 ft)—the region is a cold, arid desert that is only 20% covered with steppe and meadow vegetation. The area has been relatively free from human development due to the hostile climate and unsuitability for agriculture. The ecosystem is relatively intact, and supports herds of wild antelope, sheep, deer, and gazelles.
The Qilian Mountains subalpine meadows ecoregion covers the high meadows and shrubland of the Qilian Mountains, on the northeastern edge of the Tibetan Plateau in central China. These mountains form a divide between the dry regions of the Gobi Desert to the north, and the Qaidam Basin and the Tibetan Plateau to the south. While the habitat supports populations of marmots, grouse and some rare mammal species, the grasslands of the region are under pressure from over-grazing by domestic livestock.
The North Tibetan Plateau-Kunlun Mountains alpine desert ecoregion covers a long stretch of mostly treeless alpine terrain across the northern edge of the Tibet Plateau. A variety of cold, dry habitats are found, including alpine meadows, steppe, desert, and cushion plant floral areas.
The Tibetan Plateau alpine shrublands and meadows ecoregion covers the middle transition zone between the northern and southern regions of the Tibetan Plateau. The region supports both cold alpine steppe and meadows across a broad expanse of the plateau. Wild deer, antelope, and sheep roam the grasslands, but the habitat is increasingly being used to graze domestic livestock.
The Alai-Western Tian Shan steppe ecoregion covers the foothills on the western edge of the Tien Shan and Alay Mountains of Central Asia. This territory is mostly in southeastern Uzbekistan, with a portion running north into Kazakhstan on the east side of the Syr Darya River, and a small portion in Turkmenistan.
The Gissaro-Alai open woodlands ecoregion covers the western foothills winding around two western offshoots of the Tian Shan Mountains in western Tajikistan, and parts of eastern Uzbekistan and western Kyrgyzstan, in Central Asia. The woodlands are typically of Juniper trees and shrubs, fitting the altitude zone situated between the desert valley floor, and the tree line, above which the mountain ridges are glaciated and barren.
The Hindu Kush alpine meadow ecoregion covers a portion of the Hindu Kush Mountain Range in northern Afghanistan. Most of the terrain is between 3,000 and 4,000 meters in elevation. This portion of the Hindu Kush is very mountainous, with steep slopes. About half of the alpine meadow is bare rock or gravely soils with sparse vegetation. The remainder supports herbaceous cover of grasses and cushion plants. Human habitation is scarce and follows the river courses in the valleys.
The Paropamisus xeric woodlands ecoregion covers the portion of northeastern Afghanistan north of the central mountain range and the Hindu Kush Mountains. The name is derived from the Old Persian name for the region, Parupraesanna. While there are low canopy woodlands in the northeast of the ecorgegion, most of the territory is desert or xeric (dry) scrubland.
The Baluchistan xeric woodlands ecoregion covers the middle elevations of a series of mountain ranges of western Pakistan and northeastern Afghanistan, reaching 1,200 kilometres (750 mi) from the Arabian Sea in the south to the Hindu Kush Mountains and the Himalayas in the north. The characteristic vegetation is xeric (dry) woodlands of shrubs and herbaceous cover. The region has rich biodiversity but relatively few endemic species.
The Sulaiman Range alpine meadows ecoregion covers a series of higher altitude mountain ranges along the crest of the Sulaiman Mountains, a southerly extension of the Hindu Kush Mountains along the Afghanistan-Pakistan border. The area is relatively undeveloped, with about a third of the terrain either forested or in 'alpine steppe' shrub or herbaceous cover.
