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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 ...
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Naryn
Naryn ( ky, Нарын, translit=Naryn, Mongolian : Нарийн, Nariin, Traditional Mongolian ᠨᠠᠷᠢᠨ) is the regional administrative center of Naryn Region in central Kyrgyzstan. Its area is , and its estimated population was 41,178 as of January 2021. The town was established as a fortress on the caravan route in 1868. It is situated on both banks of the river Naryn (one of the main head waters of the Syr Darya), which cuts a picturesque gorge through the town. The city has two regional museums and some hotels, but is otherwise residential. History Naryn was established as a fortress on the important caravan route between Kashgar and Zhetysu (Semirechye) at the direction of the first Governor-General of Russian Turkestan Konstantin Petrovich von Kaufmann in 1868. Overview From Naryn, the main road (one of the branches of the ancient Silk Road) runs south through the sparsely settled central Kyrgyz highlands to the Torugart Pass and China. At present, this is the ...
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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 Province
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 cons ...
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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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Tien 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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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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