Pamir-Alay
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Pamir-Alay
The Pamir-Alay (also ''Pamiro-Alay'', russian: Памиро-Алай) is a mountain system in Tajikistan, Kyrgyzstan and Uzbekistan, encompassing four main mountain ranges extending west from the Tian Shan Mountains, and located north of the main range of Pamir. They are variously considered part of the Tian Shan, of the Pamir, or a separate mountain system. The term "Pamiro-Alay" is also used to refer to the mountain region encompassing the Pamir, the Pamir-Alay proper (then referred to as "Gissaro-Alay") and the Tajik Depression.Гиссаро-Алай
The Pamir-Alay stretches between the valleys of the rivers

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Zarafshan Range
The Zarafshan Range (russian: Зеравшанский хребет, ''Zeravšanskij hrebet''; tg, Зарафшон; uz, Zarafshon; also Zeravshan or Zarafshon; from Persian ''Zar-afshān'', meaning "the sprayer of gold") is a mountain range in Tajikistan and Uzbekistan, part of the Pamir-Alay mountains. Almost all of the range belongs to the drainage basins of the Zarafshan River. The Persian name is believed to possibly be a reference to gold found in bed of the Zarafshan River and its tributaries, which has ushered prosperity to the region from ancient times. Geography and geology The range extends over in an east−west direction along the south of Sughd Region in Tajikistan, reaching the highest point of (Chimtarga Peak) in its central part. South-west of Panjakent the range crosses from Tajikistan into Uzbekistan, where it continues at decreasing elevations () along the internal border between Samarkand and Kashkadarya Regions provinces, until it blends into ...
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Pik Skalisty (Kyrgyzstan)
Pik Skalisty (russian: Пик Скалистый; ky, Аскалы чокусу) is the highest peak in the Kara-Bel Range, Pamir-Alay. It is located in the Batken Region of Kyrgyzstan, 7 km from the border of Tajikistan. See also *List of Ultras of Central Asia *Pamir Mountains The Pamir Mountains are a mountain range between Central Asia and Pakistan. It is located at a junction with other notable mountains, namely the Tian Shan, Karakoram, Kunlun, Hindu Kush and the Himalaya mountain ranges. They are among the world ... References Mountains of Kyrgyzstan Five-thousanders {{Kyrgyzstan-geo-stub ...
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Fann Mountains
The Fann Mountains ( tg, Кӯҳҳои Фон) are part of the western Pamir-Alay mountain system in Tajikistan's Sughd Province, between the Zarafshan Range to the north and the Gissar Range to the south. In an east-west direction, they extend from the Fan Darya to the Archimaydan River. Peaks, lakes and access The Fanns boast about a hundred peaks, with several rising to altitudes of more than 5,000 meters and relative elevations of up to 1,500 meters. The highest point in Fann Mountains is Chimtarga peak (5,489 m). Other 5,000-meter peaks are Bodkhona (5,138 m), Chapdara (5,050 m), Big Hansa, Little Hansa (5,031 m), Zamok ('5,070 m), Mirali (5,132 m), and Energia (5,120 m). There are many lakes in the Fanns.The best known are Alaudin lakes in the Chapdara River valley, Kulikalon Lakes on the northern slope of Chimtarga peak, Big Allo Lake and Iskanderkul Lake. There is a stunning mountain range in Western Tajikistan, near the city of Punjikent, which surprises tourists with i ...
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Alay Range
The Alay or Alai Range ( ky, Алай тоо кыркасы; russian: Алайский хребет) is a mountain range that extends from the Tien Shan mountain range in Kyrgyzstan west into Tajikistan. It is part of the Pamir-Alay mountain system. The range runs approximately east to west. Its highest summit is Pik Tandykul (russian: пик Тандыкуль), reaching 5544 m. It forms the southern border of the Fergana Valley, and in the south it falls steeply to the Alay Valley.Алайский хребет
The southern slopes of the range drain into the Kyzylsuu or



Köýtendag Range
Köýtendag Range (also Koytendag Range or Kugitangtau Range, tk, Köýtendag) is a spur of the Pamir-Alay mountains in the south-east of Turkmenistan, extending along the border with Uzbekistan's Surxondaryo Region Surxondaryo Region ( uz, Surxondaryo viloyati, Сурхондарё вилояти, سرخان‌دریا ولایت, russian: Сурхандарьинская область, fa, سرخان‌دریا, UniPers: "sorxāndaryā"), old spelling Su .... It rises to at Mount Aýrybaba, which is the highest summit in Turkmenistan. The Köýtendag Nature Reserve is located within the range. References "Kugitangtau" ''Encyclopædia Britannica Online'', 2008. Retrieved on 2008-12-28. ''Big Soviet Encyclopedia Online'' . Retrieved on 2008-12-28. Nature reserve in Koytendag Mountains Mountains of Turkmenistan Mountain ranges of Uzbekistan {{Turkmenistan-geo-stub ...
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Gissar Range
Hisar Range ( tg, Қаторкӯҳи Ҳисор; uz, Hisor tizmasi, russian: Гиссарский хребет; uk, Ґаторкугі Гісор; fa, رشته‌کوه حصار; also known as Hissar, Hisor, or Gissar Range) is a mountain range in Central Asia, in the western part of the Pamir-Alay system, stretching over 200 km in the general east–west direction across the territory of Tajikistan and Uzbekistan. Geography The Hisar Range lies south of the Zarafshon Range, extending north of Dushanbe through Tajikistan's Hissar District of the Districts of Republican Subordination and reaching Uzbekistan at the north tip of Surxondaryo Region. The highest point in the Hissar Range at is located in Uzbekistan on the border with Tajikistan, just north-west of Dushanbe. Formerly known as ''Peak of the 22nd Congress of the Communist Party'', the Khazret Sultan is also the highest point in all Uzbekistan. The Hissar Range is composed of crystalline rocks, schist, and sandst ...
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Turkestan Range
One of the northern extensions of the Pamir-Alay system, the Turkestan Range (russian: Туркестанский хребет; ky, Түркстан кырка тоосу; uz, Туркистон тизмаси, Turkiston tizmasi; tg, Қаторкӯҳи Туркистон) stretches for a total length of 340 km from the Alay Mountains on the border of Kyrgyzstan with Tajikistan to the Samarkand oasis in Uzbekistan. It runs in the east–west direction, north of the Zeravshan Range, forming the southern boundary of the Ferghana Valley in Tajikistan and Golodnaya Steppe in Uzbekistan. The highest elevations are in the east, near the border with Kyrgyzstan. The maximum elevation is the Pik Skalisty at . Glaciation occurs especially in the east. The southern slopes are bare cliffs and mountain steppe; the northern slopes are covered with forests. A highway through the Shakhristan Pass at connects the capital Dushanbe with Khujand in Northern Tajikistan (Sughd Province). See ...
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Fergana Valley
The Fergana Valley (; ; ) in Central Asia lies mainly in eastern Uzbekistan, but also extends into southern Kyrgyzstan and northern Tajikistan. Divided into three republics of the former Soviet Union, the valley is ethnically diverse and in the early 21st century was the scene of conflict. A large triangular valley in what is an often dry part of Central Asia, the Fergana owes its fertility to two rivers, the Naryn River, Naryn and the Kara Darya, which run from the east, joining near Namangan, forming the Syr Darya river. The valley's history stretches back over 2,300 years, when Alexander the Great founded Alexandria Eschate at its southwestern end. Chinese chroniclers date its towns to more than 2,100 years ago, as a path between Greek, Chinese, Bactrian and Parthian civilisations. It was home to Babur, founder of the Mughal Dynasty, tying the region to modern Afghanistan and South Asia. The Russian Empire conquered the valley at the end of the 19th century, and it became part ...
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Mountain Ranges Of Kyrgyzstan
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Mountain Ranges Of Tajikistan
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Pik Skalisty
Pik Skalisty (russian: Пик Скалистый) is the highest peak in the Shughnon Range, Pamir. It is located in the Gorno-Badakhshan Autonomous Province of Tajikistan. See also *List of mountains of Tajikistan Peaks ;Pamir-Alay * Pamir Mountains ** Academy of Sciences Range *** Ismoil Somoni Peak *** Peak Korzhenevskaya (Ozodi) *** Mount Garmo ** Rushan Range *** Patkhor Peak ** Shakhdara Range *** Mayakovskiy Peak *** Karl Marx Peak ** Trans-Ala ... References Mountains of Tajikistan Gorno-Badakhshan Autonomous Region Five-thousanders {{Tajikistan-geo-stub ...
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Vakhsh River
The Vakhsh (Russian and Tajik: Вахш - ''Vaxsh'', fa, وخش), also known as the Surkhob (Сурхоб, سرخاب), in north-central Tajikistan, and the Kyzyl-Suu ( ky, Кызыл-Суу), in Kyrgyzstan, is a Central Asian river, and one of the main rivers of Tajikistan. It is a tributary of the Amu Darya river."Tajikistan - Topography and Drainage"
in Tajikistan: a Country Study (Washington: Library of Congress, 1996)


Geography

The river flows through the , passing through very mountainous territory that frequently restricts its flow to narrow channels within deep gorges. Some of the largest glaciers in Tajikistan, including the
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