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Jaman-Too
The Jaman-Too (, , or , and also known as Arpanyn Ala-Toosuu) is a range in the south-west of the Internal Tien-Shan. In the east, the range adjoins Fergana Range. It stretches for a length of with a width of . The average elevation is approximately , and the highest elevation of . The southern slopes are steep, and northern - gentle. The mountains are composed of limestone, sandstone Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sand ..., and dolomite. References Mountain ranges of Kyrgyzstan Mountain ranges of the Tian Shan {{Kyrgyzstan-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
At-Bashy District
At-Bashy () is a district of Naryn Region in Kyrgyzstan established in its present borders in 1930. The administrative center is at At-Bashy. Its area is , and its resident population was 55,771 in 2021. The mountain lake Chatyr-Kul lies in the southwestern part of the district. Geography Topography The At-Bashy District is in the southern part of the Naryn Region and it is limited from the north by the Baybiche Too, Naryn Too, and Jaman-Too, from the south by Torugart-Too and Kakshaal Too, and from the west by the Fergana Range. Among other mountain ranges of the district are At-Bashy Range and Jangy Jer. The difference in absolute elevations in the mountainous areas varies from , and in the valleys from . In the eastern part of the region, near the border with China, there is the maximum absolute elevation of Dankov Peak - . Hydrology The hydrographic network is represented by the rivers of the Naryn basin - the At-Bashy (river) with an annual average flow rate of 41. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kyrgyzstan
Kyrgyzstan, officially the Kyrgyz Republic, is a landlocked country in Central Asia lying in the Tian Shan and Pamir Mountains, Pamir mountain ranges. Bishkek is the Capital city, capital and List of cities in Kyrgyzstan, largest city. Kyrgyzstan is bordered by Kazakhstan to the Kazakhstan–Kyrgyzstan border, north, Uzbekistan to the Kyrgyzstan–Uzbekistan border, west, Tajikistan to the Kyrgyzstan–Tajikistan border, south, and China to the China–Kyrgyzstan border, east and southeast. Ethnic Kyrgyz people, Kyrgyz make up the majority of the country's over 7 million people, followed by significant minorities of Uzbeks and Russians. 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 unde ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Naryn Region
Naryn Region is the largest region 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 Lake Issyk-Kul. It is known as the location of Lake Song-Köl, Lake Chatyr-Köl, 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. It boasts mountains, alpine pastures, and Song Köl Lake which during summer months attracts large herds of sheep and horses with their h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tien-Shan
The Tian Shan, also known as the Tengri Tagh or Tengir-Too, meaning the "Mountains of God/Heaven", is a large system of mountain ranges in Central Asia. The highest peak is Jengish Chokusu at high and located in Kyrgyzstan. Its lowest point is at the Turpan Depression, which is below sea level. The Tian Shan is sacred in Tengrism. Its second-highest peak is known as Khan Tengri, which can be translated as "Lord of the Spirits". At the 2013 Conference on World Heritage, the eastern portion of Tian Shan in western China's Xinjiang Region was listed as a World Heritage Site. The western portion in Kyrgyzstan, Kazakhstan, and Uzbekistan was then listed in 2016. Geography Tian Shan with the ancient Silk Road The Tian Shan range is located north and west of the Taklamakan Desert and directly north of the Tarim Basin. It straddles the border regions of Kazakhstan, Kyrgyzstan, Uzbekistan and Xinjiang in Northwest China. To the south, it connects with the Pamir Mountains, while ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fergana Range
The Fergana Range (; ) is a mountain range of the Tian Shan in the Kyrgyz Republic. The length of the range is 206 km, and the average height is 3,600 m above sea level. The highest mountain is 4,893 m above sea level. Geography The Fergana Range stretches from north-west to south-east, separating the Fergana Valley and the inner Tian Shan. The south-east section of the range is higher. It joins the Torugart Ridge and the Alaykuu Ridge via the Söök Pass (Naryn Region), Söök Pass (4024 m). The South-west slope is long and low-sloped, the north-east - short and steep. Mountain ranges southwest are denoted by collective term: Pamir-Alay system. Geology The Fergana Range is composed of schist, sandstone, limestone, and other sedimentary metamorphic formations ruptured by intrusions of gabbro and diabase. References Mountain ranges of Kyrgyzstan Naryn Region Osh Region Jalal-Abad Region Mountain ranges of the Tian Shan {{kyrgyzstan-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary rock, sedimentary carbonate rock that contains a high percentage of the mineral Dolomite (mineral), dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). One of the first geologists to distinguish dolomite from limestone was Déodat Gratet de Dolomieu, a French mineralogist and geologist after whom it is named. He recognized and described the distinct characteristics of dolomite in the late 18th century, differentiating it from limestone. Most dolomite was formed as a magnesium replacement of limestone or of Lime (mineral), lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the v ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 area, and is usually higher than a hill, typically rising at least 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 climate, mountains t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
