Suusamyr Too
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Suusamyr Too
Suusamyr Too ( ky, Суусамыр тоо кыркасы) is a mountain range in internal Tian Shan in Kyrgyzstan. It separates Suusamyr Valley and Toluk Saragat Valley. The length of the range is 126 km, and height up to 4048m. It is composed of granite, and schist of lower Paleozoic The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ' .... References Mountain ranges of Kyrgyzstan Naryn Region Osh Region Jalal-Abad Region Mountain ranges of the Tian Shan {{kyrgyzstan-geo-stub ...
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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 in the ...
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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 is co ...
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Jalal-Abad Region
Jalal-Abad Region ( ky, Жалал-Абад облусу, Jalal-Abad oblusu; russian: Джалал-Абадская область, Dzhalal-Abadskaya oblast) is a region (''oblast'') of Kyrgyzstan. Its capital is the city of the same name, Jalal-Abad. It is surrounded by (clockwise from the north) Talas Region, Chüy Region, Naryn Region, Osh Region, and Uzbekistan. Jalal-Abad Region was established on 21 November 1939. On 27 January 1959 it became a part of Osh Region, but regained its old status as a region on 14 December 1990. Its total area is . The resident population of the region was 1,260,617 as of January 2021. The region has a sizeable Uzbek (24.8% in 2009) minority. Geography Jalal-Abad Region covers (16.2% of total country's area) in central-western Kyrgyzstan. The southern edge of the region is part of the Ferghana Valley. The rest of the region is mountainous. M41, the main north-south highway from Bishkek to Osh, takes a very crooked route down the center o ...
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Jumgal District
Jumgal ( ky, Жумгал району, Jumgal rayonu) is a district of Naryn Region in central 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 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:
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Toktogul District
Toktogul ( ky, Токтогул району) is a district of Jalal-Abad Region in western Kyrgyzstan. The administrative seat lies at Toktogul. Its area is , and its resident population was 103,310 in 2021. The town and district are named after its most famous son - the musician Toktogul Satylganov. The Toktogul reservoir is a geographical feature of the district and the capital lies on the north shore. Geography The district is located in the southern part of the region within the Naryn river valley. It is bordered by Talas Alatau and Suusamyr Too on the north, At-Oynok Range on the west, and by complex system of mountains: Babash-Ata, Fergana Range and Kekirim-Too on the south. Mountain areas are characterized by highly dissected topography. Absolute elevations of ranges reach 4,165m (Uzun-Akhmat mountains) and 4351 m (Kekirim-Too). The valley is at 650-850 m above sea level. Mountains occupy 93%, and valley - 7% of the district. The hydrology is dominated by Naryn river, To ...
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Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ...
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Paleozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean ...
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Tian Shan
The Tian Shan,, , otk, 𐰴𐰣 𐱅𐰭𐰼𐰃, , tr, Tanrı Dağı, mn, Тэнгэр уул, , ug, تەڭرىتاغ, , , kk, Тәңіртауы / Алатау, , , ky, Теңир-Тоо / Ала-Тоо, , , uz, Tyan-Shan / Tangritog‘, , also known as the Tengri Tagh or Tengir-Too, meaning the ''Mountains of Heaven'' or the ''Heavenly Mountain'', is a large system of mountain ranges located in Central Asia. The highest peak in the Tian Shan is Jengish Chokusu, at high. Its lowest point is the Turpan Depression, which is below sea level. One of the earliest historical references to these mountains may be related to the Xiongnu word ''Qilian'' ( zh, s=祁连, t=祁連, first=t, p=Qílián) – according to Tang commentator Yan Shigu, ''Qilian'' is the Xiongnu word for sky or heaven. Sima Qian in the ''Records of the Grand Historian'' mentioned ''Qilian'' in relation to the homeland of the Yuezhi and the term is believed to refer to the Tian Shan rather than the Qilia ...
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Toluk Saragat Valley
Toluk is a village in Jalal-Abad Region of Kyrgyzstan. It is part of the Toktogul District Toktogul ( ky, Токтогул району) is a district of Jalal-Abad Region in western Kyrgyzstan. The administrative seat lies at Toktogul. Its area is , and its resident population was 103,310 in 2021. The town and district are named after .... Its population was 1,304 in 2021. References Populated places in Jalal-Abad Region {{JalalAbad-geo-stub ...
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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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