Hissar Mountains
The Hisar Range, formerly the Gissar Range, is a mountain range in Central Asia, in the western part of the Pamir-Alay system, stretching over 200 km in the general east–west direction across the territory of Tajikistan and Uzbekistan. Geography The Hisar Range lies south of the Zarafshon Range, extending north of Dushanbe through Tajikistan's Hissar District of the Districts of Republican Subordination and reaching Uzbekistan at the north tip of Surxondaryo Region. The highest point in the Hissar Range is Alpomish Peak, confirmed when a 2023 survey determined nearby Khazret Sultan to be shorter. With an elevation of , the mountain is located on the Uzbekistan-Tajikistan border, just north-west of Dushanbe, and is also the highest point in Uzbekistan. The Hissar Range is composed of crystalline rocks, schist, and sandstone, punctured by granite intrusions. Nature Hissor Valley, which encompasses the Shirkent National Park is a reserve, which is expected to be expa ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Anzob Pass
Anzob ( Tajik: Анзоб) is a village and jamoat in north-west Tajikistan. It is located in Ayni District in Sughd Region, in the Zarafshan Range, about north of Dushanbe. The jamoat has a total population of 8,238 (2015).Jamoat-level basic indicators United Nations Development Programme in Tajikistan, accessed 5 October 2020 It is located on the M34 highway and in the Yaghnob River . Anzob has a mining and beneficiation complex. The Jamoat consists of 23 villages, ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Surxondaryo Region
Surxondaryo Region is a region ('' viloyat'') of Uzbekistan, located in the extreme south-east of the country. Established on 6 March 1941, it borders on Qashqadaryo Region internally, and Turkmenistan, Afghanistan and Tajikistan externally, going anticlockwise from the north. It takes its name from the river Surxondaryo, that flows through the region. It covers an area of 20,100 km². The population is estimated at 2,743,201 (beginning of 2022 data), with 80% living in rural areas.''Statistical Yearbook of the Regions of Uzbekistan 2005'', State Statistical Committee, Tashkent, 2006 (Russian). According to official data, 83% of the population are Uzbeks and 12,5% Tajiks, but several sources argue that the Tajik population might be significantly higher in this region (bitter debates accompanied the Soviet allocation of Surkhandarya Region to the Uzbek SSR rather than the Tajik SSR in 1929, as that region, as well as the areas of Bukhara and Samarkand, had sizable, if not domi ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountain Ranges Of Uzbekistan
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 te ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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List Of Mountains In Tajikistan ...
Peaks ;Pamir-Alay * Pamir Mountains ** Academy of Sciences Range *** Ismoil Somoni Peak *** Peak Korzhenevskaya (Ozodi) *** Mount Garmo ** Rushan Range *** Patkhor Peak ** Shakhdara Range *** Mayakovskiy Peak *** Karl Marx Peak ** Trans-Alay Range *** Ibn Sina Peak (Lenin) ** Yazgulem Range *** Independence Peak (Revolution) ** Peter I Range *** Moscow Peak ** Gissar Range ***Khazret Sultan ** Shughnon Range *** Pik Skalisty * Alay Mountains * Fann Mountains * Zeravshan Range ** Chimtarga Peak * Concord Peak ;Tian Shan * Turkestan Range * Vakhsh Range {{Authority control * * Tajikistan Mountains Tajikistan Tajikistan, officially the Republic of Tajikistan, is a landlocked country in Central Asia. Dushanbe is the capital city, capital and most populous city. Tajikistan borders Afghanistan to the Afghanistan–Tajikistan border, south, Uzbekistan to ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, 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 dike (geology), 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 diagram, 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) conta ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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Schist
Schist ( ) is a medium-grained metamorphic rock generally derived from fine-grained sedimentary rock, like shale. It shows pronounced ''schistosity'' (named for the rock). 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 mica, 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 schis ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Crystalline Rock
A crystal or crystalline solid is a solid material whose constituents (such as atoms, molecules, or ions) are arranged in a highly ordered microscopic structure, forming a crystal lattice that extends in all directions. In addition, macroscopic single crystals are usually identifiable by their geometrical shape, consisting of flat faces with specific, characteristic orientations. The scientific study of crystals and crystal formation is known as crystallography. The process of crystal formation via mechanisms of crystal growth is called crystallization or solidification. The word ''crystal'' derives from the Ancient Greek word (), meaning both "ice" and "rock crystal", from (), "icy cold, frost". Examples of large crystals include snowflakes, diamonds, and table salt. Most inorganic solids are not crystals but polycrystals, i.e. many microscopic crystals fused together into a single solid. Polycrystals include most metals, rocks, ceramics, and ice. A third category of so ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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List Of Elevation Extremes By Country
The following sortable table lists land surface elevation extremes by country or dependent territory. Topographic elevation is the vertical distance above the reference geoid, a mathematical model of the Earth's sea level as an equipotential gravitational surface. Table National elevation ranges Of all countries, Lesotho has the world's highest low point at . Other countries with high low points include Rwanda and Andorra . Countries with very low high points include Maldives , Tuvalu, and the Marshall Islands . These island countries also have the smallest range between their lowest (sea level) and highest points, and are very sensitive to changes in sea level. The highest and lowest points in China constitute the greatest elevation range within any single country at . The elevation ranges are also great in Nepal , Pakistan , and India . Monaco's elevation range is among the greatest relative to surface area. Within its 2.02 km2 territory, there is a differen ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Khazret Sultan
Khazret Sultan ( Uzbek: ) is a mountain in Uzbekistan, with an elevation of . It is considered to be the highest point in this country. The mountain is located on the border of Uzbekistan's Surkhondaryo Region and Tajikistan's Sughd Region Sughd Province, also referred to as the Sogdia Region, and Leninabad before 2001, is one of the four administrative divisions and one of the three provinces that make up Tajikistan. Centered in the historical Sogdiana, it is located in the north ..., in the Gissar Range. The mountain was formerly known as "''Peak of the 22nd Congress of the Communist Party''". See also * Geography of Uzbekistan * List of mountains of Tajikistan References External links *Central Asia Mountain Climbing Central Asia Mountaineering Agency. *Initial Communication of the Republic of Uzbekistan - Geographic Situation and Climate, page 17 Mountains of Tajikistan Mountains of Uzbekistan Tajikistan–Uzbekistan border International mountains of ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Districts Of Republican Subordination
Districts under Tajikistan Central Government Jurisdiction, also translated as Districts of Republican Subordination or Districts under Republic(an) Subordination (; , Latin Tajik alphabet: ), is a region in Tajikistan, consisting of 9 districts and 4 district-level cities that are directly under central administration. Dushanbe, the capital of Tajikistan, is surrounded by the Districts under Central Government Jurisdiction, but not part of it. The region shares a border with Dushanbe, Sughd, GBAO, Khatlon, Kyrgyzstan ( Batken and Osh regions) and Uzbekistan ( Surxondaryo). The region covers an area of 28,500 square kilometres, and has a total population of 2,165,900 (2020). The Districts' ethnic composition in 2010 was 85% Tajik and 11.7% Uzbek. History After the dissolution of Stalinabad Oblast in 1951, the territories of the former province became directly subordinate to the government of the Tajik SSR, which is how the name came about. In 1955, the Gharm Oblast was di ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |