Ming-Kush Valley
The Ming-Kush Valley ( ky, Миңкуш өрөөнү) is a valley located in Jumgal District of Naryn Region in central Kyrgyzstan. It is separated from the Naryn river valley to the south by the Moldo Too range. The Kabak Too range lies to its north. The valley is long and wide. The river Ming-Kush (a left tributary of the Kökömeren) flows through it, and the main settlement is the village Ming-Kush Ming-Kush ( ky, Миң-Куш, lit=a thousand birds) is a village (urban-type settlement from 1953 until 2012) in the Jumgal District of Naryn Region of Kyrgyzstan. Its population was 3,647 in 2021. It is located in the narrow Ming-Kush Valley at .... Coal deposits in the valley have been exploited since the 1950s. References {{reflist Valleys of Kyrgyzstan Naryn Region ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Kyrgyzstan
Kyrgyzstan,, pronounced or the Kyrgyz Republic, is a landlocked country in Central Asia. Kyrgyzstan is bordered by Kazakhstan to the north, Uzbekistan to the west, Tajikistan to the south, and the People's Republic of China to the east. Its capital and largest city is Bishkek. Ethnic Kyrgyz make up the majority of the country's seven million people, followed by significant minorities of Uzbeks and Russians. The Kyrgyz language is closely related to other Turkic languages. Kyrgyzstan's history spans a variety of cultures and empires. Although geographically isolated by its highly mountainous terrain, Kyrgyzstan has been at the crossroads of several great civilizations as part of the Silk Road along with other commercial routes. Inhabited by a succession of tribes and clans, Kyrgyzstan has periodically fallen under larger domination. Turkic nomads, who trace their ancestry to many Turkic states. It was first established as the Yenisei Kyrgyz Khaganate later i ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Naryn Region
Naryn Region ( ky, Нарын облусу, Naryn oblusu; russian: Нарынская область, Narynskaya oblast) is the largest region ('' oblus'') of Kyrgyzstan. It is located in the east of the country and borders with Chüy Region in the north, Issyk-Kul Region in the northeast, Xinjiang Uyghur Autonomous Region of China in the southeast, Osh Region in the southwest, and Jalal-Abad Region in the west. Its capital is Naryn. Its total area is . The resident population of the region was 292,140 as of January 2021. The main highway runs from the Chinese border at Torugart Pass north to Balykchy on Issyk-Kul Lake. It is known as the location of Song Köl Lake and Chatyr-Kul Lake and Tash Rabat. The population of Naryn oblast is 99% Kyrgyz. The economy is dominated by animal herding (sheep, horses, yaks), with wool and meat as the main products. Mining of various minerals developed during the Soviet era has largely been abandoned as uneconomical. Today the oblast ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Jumgal District
Jumgal ( ky, Жумгал району, Jumgal rayonu) is a district of Naryn Region in central Kyrgyzstan. The administrative seat lies at Chaek. Its area is , and its resident population was 44,866 in 2021. It is a mountainous district. Its main rivers are the Kökömeren (a tributary to the river Naryn) and its tributaries Jumgal, Suusamyr and Batysh Karakol. Population Populated places In total, Jumgal District include 30 settlements in 13 rural communities ('). Each rural community includes one or several villages. The rural communities and settlements in the Jumgal District are as follows:List of Rural Communities of Kyrgyzstan [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Valley
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Naryn (river)
The Naryn ( ky, Нарын, uz, Norin) rises in the Tian Shan mountains in Kyrgyzstan, Central Asia, flowing west through the Fergana Valley into Uzbekistan. Here it merges with the Kara Darya (near Namangan) to form the Syr Darya. It is long (together with its upper course Chong-Naryn) and its basin area is . It has an annual flow of . The river contains many reservoirs which are important in the generation of hydroelectricity. The largest of these is the Toktogul Reservoir in Kyrgyzstan containing of water. Dams downstream of the Toktogul in Kyrgyzstan include: Kürpsay, Tash-Kömür, Shamaldy-Say and Üch-Korgon. Upstream of Toktogul in Kyrgyzstan is the Kambar-Ata-2 and At-Bashy Dams while the Kambar-Ata-1 Dam is in planning stages. Some places along the river: Kyrgyzstan: Kara-Say (see Barskoon), Naryn Region, Naryn, Dostuk, Jalal-Abad Region, Kazarman, Toktogul Reservoir, Kara-Köl, Tash-Kömür. Tributaries The main tributaries of the Naryn are, from s ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Moldo Too
The Moldo Too ( ky, Молдотоо) is a range in the inner Tien Shan, Kyrgyzstan Kyrgyzstan,, pronounced or the Kyrgyz Republic, is a landlocked country in Central Asia. Kyrgyzstan is bordered by Kazakhstan to the north, Uzbekistan to the west, Tajikistan to the south, and the People's Republic of China to the ea .... The length of the range is approximately 110 km and the width - 26 km. The average altitude is about 3,600 m and the highest peak - 4,185 m. The range is mainly composed of sedimentary rocks of Middle Paleozoic. References Mountain ranges of Kyrgyzstan Mountain ranges of the Tian Shan {{Kyrgyzstan-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Kabak Too
Kabak Too is a mountain range in the inner Tian Shan in Naryn Region, Kyrgyzstan Kyrgyzstan,, pronounced or the Kyrgyz Republic, is a landlocked country in Central Asia. Kyrgyzstan is bordered by Kazakhstan to the north, Uzbekistan to the west, Tajikistan to the south, and the People's Republic of China to the east. .... It is located between Jumgal and Ming-Kush valleys. The length of the range is about 40 km, width - up to 16 km. The highest point is Kashkasuu Chokusu - . References Mountain ranges of Kyrgyzstan Naryn Region {{kyrgyzstan-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ming-Kush (river)
The Ming-Kush ( ky, Миңкуш or Миң-Куш; russian: Мин-Куш) is a river in Jumgal District of Naryn Region of Kyrgyzstan. It rises on north slopes of Moldo Too and flows into Kökömeren The Kökömeren ( ky, Көкөмерен) is a right tributary of the Naryn located in Chüy Region (Jayyl District) and Naryn Region (Jumgal District) of Kyrgyzstan. It is formed by the confluence of the rivers Suusamyr and Batysh Karakol (Weste ... river from the left. The length of the river is and the basin area . Average annual discharge is . The maximum discharge is in June - July and the minimum in January - February. The river is majorly fed by springs (42%), glaciers (28%) and snow (25.4%). References Rivers of Kyrgyzstan {{Kyrgyzstan-river-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Kökömeren
The Kökömeren ( ky, Көкөмерен) is a right tributary of the Naryn located in Chüy Region (Jayyl District) and Naryn Region (Jumgal District) of Kyrgyzstan. It is formed by the confluence of the rivers Suusamyr and Batysh Karakol (Western Karakol). It is long, and has a drainage basin of , with an average discharge of . It possesses significant hydro-power potential. In June 2011, China and Kyrgyzstan signed a protocol of intent to begin construction of Kökömeren River chain of power plants in 2012. Whitewater rafting Rafting and whitewater rafting are recreational outdoor activities which use an inflatable raft to navigate a river or other body of water. This is often done on whitewater or different degrees of rough water. Dealing with risk is often a ... and fishing are popular tourist activities on the Kökömeren. References Rivers of Kyrgyzstan {{Kyrgyzstan-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Ming-Kush
Ming-Kush ( ky, Миң-Куш, lit=a thousand birds) is a village (urban-type settlement from 1953 until 2012) in the Jumgal District of Naryn Region of Kyrgyzstan. Its population was 3,647 in 2021. It is located in the narrow Ming-Kush Valley at the right bank of the river Ming-Kush, about south of Chaek Chaek ( ky, Чаек) is a village in Naryn Region of Kyrgyzstan on the A361 highway which crosses the north of the region. Its population was 3,762 in 2021. It is the center of the Jumgal District. It is about 100km west of Kochkor and 45km we .... It is the site of a former uranium mine. Population References Populated places in Naryn Region {{Naryn-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Valleys Of Kyrgyzstan
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |