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Tajikistan

Pamir Mountains

The Pamir Mountains are a mountain range in Central Asia at the junction of the Himalayas with the Tian Shan, Karakoram, Kunlun, and Hindu Kush ranges. They are among the world’s highest mountains, and since Victorian times, they have been known as the "Roof of the World", presumably a translation from Persian. In other languages they are called: Kyrgyz Памир тоолору Pamir Toolori; Persian: رشته کوه های پامیر‎ Reshte Kūh-hāye Pāmīr; Tajik: Ришта Кӯҳҳои Помир Rishta Kuhhoyi Pomir; Pashto: د پامير غرونه‎ Da Pamir Ghruna; Uyghur: پامىر ئېگىزلىكى Pamir Ezgizliki; Urdu: پامیر کوهستان Pamir Kuhestan; simplified Chinese: 葱岭; traditional Chinese: 蔥嶺; pinyin: Cōnglǐng; Wade–Giles: Ts'ung-ling or "Onion Range" . The name "Pamir" is used more commonly in Modern Chinese and loaned as simplified Chinese: 帕米尔; traditional Chinese: 帕米爾; pinyin: Pàmǐ'ěr. The precise extent of the Pamir Mountains is debatable. They lie mostly in Gorno-Badakhshan province of Tajikistan. To the north they join the Tian Shan mountains along the Alay Valley of Kyrgyzstan. To the south they border the Hindu Kush mountains along Afghanistan's Wakhan Corridor. To the east they are generally considered to extend to the range that includes China's Kongur Tagh, a peak which is included in the "Eastern Pamirs" more often than in the Kunlun Mountains, as Kongur Tagh and the Kunlun range are separated by the large Yarkand River valley; no valley of such significance separates the Pamirs and Kongur Tagh, just political boundaries.

Usoi Dam

The Usoi Dam is a natural landslide dam along the Murghab River in Tajikistan. At 567 metres high, it is the tallest dam in the world, either natural or man-made. The dam was created on February 18, 1911, when the 7.4-Ms Sarez earthquake caused a massive landslide that blocked the flow of the river. The dam is formed of approximately 2 cubic kilometres of rock dislodged from the steeply sloped river valley of the Murghab, which cuts from east to west through the high and rough Pamir Mountains. It is named after the village of Usoi, which was completely buried by the 1911 landslide. The dam rises to a height of 500 to 700 metres from the original valley floor. The basin formed by Usoi Dam now holds Sarez Lake, a 55.8-kilometre long lake holding 16.074 cubic kilometres of water. Water does not flow over the top of the dam, which would quickly cause it to erode away; instead, water seeps out of the base of the dam at a rate which approximately matches the rate of inflow, maintaining the lake at a relatively constant level. The flow averages about 45 cubic meters per second, and dissipates about 250 megawatts. Geologists are concerned that the Usoi Dam may become unstable during future large-magnitude earthquakes, which are relatively common in the seismically active Pamirs, and might collapse due to liquefaction or subsequent landslides during such an event. Collapse of the dam would unleash a locally catastrophic flood. The Murghabs river valley tends to be relatively narrow and steep. This would focus and maintain any floods destructive power as it swept through the valley of the Murghab District.

Tajikistan

Tajikistan (, , or ; Тоҷикистон [tɔd͡ʒikɪsˈtɔn]), officially the Republic of Tajikistan (Tajik: Ҷумҳурии Тоҷикистон, Çumhuriji Toçikiston/Jumhuriyi Tojikiston; Russian: Респу́блика Таджикистан, Respublika Tadzhikistan), is a mountainous landlocked sovereign country in Central Asia. With an estimated 8 million people in 2013, it is the 98th most populous country and with an area of 143,100 km2 (55,300 sq mi), it is the 96th largest country in the world. It is bordered by Afghanistan to the south, Uzbekistan to the west, Kyrgyzstan to the north, and China to the east. Pakistan lies to the south separated by the narrow Wakhan Corridor. Traditional homelands of Tajik people included present-day Tajikistan, Afghanistan and Uzbekistan. The territory that now constitutes Tajikistan was previously home to several ancient cultures, including the city of Sarazm of the Neolithic and the Bronze Age, and was later home to kingdoms ruled by people of different faiths and cultures, including the Oxus civilization, Andronovo culture, Buddhism, Nestorian Christianity, Zoroastrianism, and Manichaeism. The area has been ruled by numerous empires and dynasties, including the Achaemenid Empire, Sassanian Empire, Hephthalite Empire, Samanid Empire, Mongol Empire, Timurid dynasty, and the Russian Empire. As a result of the breakup of the Soviet Union, Tajikistan became an independent nation in 1991. A civil war was fought almost immediately after independence, lasting from 1992 to 1997. Since the end of the war, newly established political stability and foreign aid have allowed the country's economy to grow. Tajikistan is a presidential republic consisting of four provinces. Most of Tajikistan's 8 million people belong to the Tajik ethnic group, who speak Tajik), although many people also speak Russian. Mountains cover more than 90% of the country. It has a transition economy that is highly dependent on remittances, aluminium and cotton production.

Kayrakkum Dam

The Kayrakkum Dam, also spelt variously as Kayrakum, Kairakum, Qayraqqum or Qayroqqum, is an embankment dam on the Syr Darya River near the town of Kayrakkum in Sughd Province, Tajikistan. It is situated on the western edge of the Fergana Valley and creates Kayrakkum Reservoir. The reservoir supplies water for irrigation, primarily in Uzbekistan downstream, and hydroelectric power production. The reservoir is also a Ramsar site. The dam's power station has an installed capacity of 126 MW and is operated by Barki Tojik. Construction on the dam began in 1952. It began to impound its reservoir in 1956 and the first two generators were commissioned that year. The other four were operational in 1957 and the project was complete in 1959. The power station is currently undergoing a rehabilitation which should be completed in 2020. Two new and larger turbines will increase the installed capacity to 142 MW. The 32 m tall and 1,202 m long embankment dam is filled with sand, gravel and rock. It's spillway and power station are co-located on the left side of the dam in a gravity dam section. The spillway contains six maintenance gates and six operational gates with a total discharge capacity of 3,960 m3/s . The power station houses six 21 MW Kaplan turbine-generators. Kayrakkum Reservoir has a total storage capacity of 4,200,000,000 m3 and surface of 513 km2 . Of the total reservoir capacity, 2,300,000,000 m3 can be used for irrigation downstream and/or power generation. 1,900,000,000 m3 is dead or unusable storage.

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