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Zangilan District
Zangilan District ( az, Zəngilan rayonu) is one of the 66 districts of Azerbaijan. It is located in the south-west of the country and belongs to the East Zangezur Economic Region. The district borders the districts of Qubadli, Jabrayil, the Syunik Province of Armenia and the East Azerbaijan Province of Iran. Its capital and largest city is Zangilan. As of 2020, the district had a nominal population of 45,200. Geography Zangilan city is located in the south-western part of Azerbaijan, in the northern part of the Aras River and borders upon Armenia and Iran. There exists a Mesozoic relief and cretaceous, volcanic and sedimentary rocks are spread in the territory of the district. Remains of the Jurassic and Cretaceous periods spread in mountainous territories are dated back to a period of 150-200 thousand years ago. There are Barbar and Salafir (2270 meters) summits in the territory and this mountain range passes Aras ravine near Aghbend, Vegnali. There is another mountain ran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Administrative Divisions Of Azerbaijan
Azerbaijan is administratively divided into 66 districts () and 11 cities () that are subordinate to the Republic. Out of these, 7 districts and 1 city is located within the Nakhchivan Autonomous Republic. The districts are further divided into municipalities (). Additionally, the districts of Azerbaijan are grouped into 14 Economic Regions (). On July 7, 2021, the President of Azerbaijan Ilham Aliyev signed Decree "On the new division of economic regions in the Republic of Azerbaijan". Administrative divisions Contiguous Azerbaijan The territory of former Nagorno-Karabakh Autonomous Oblast presently consists of the districts of Khojavend, Shusha, Khojaly, the eastern portion of Kalbajar and the western portion of Tartar. The Autonomous Oblast was abolished on 26 November 1991, by the Supreme Soviet of the Azerbaijan SSR. Since then, the territory of the autonomous oblast has been administratively split between the aforementioned districts. As a result of the First Nag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesozoic
The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Periods. It is characterized by the dominance of archosaurian reptiles, like the dinosaurs; an abundance of conifers and ferns; a hot greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest well-documented mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, pterosaurs, mosasaurs, and plesiosaurs. The Mesozoic was a time of significant tectonic, climatic, and evolutionary activity. The era witnessed the gradual ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
First Nagorno-Karabakh War
The First Nagorno-Karabakh War, referred to in Armenia as the Artsakh Liberation War ( hy, Արցախյան ազատամարտ, Artsakhyan azatamart) was an ethnic conflict, ethnic and territorial conflict that took place from February 1988 to May 1994, in the enclave of Nagorno-Karabakh in southwestern Azerbaijan, between the majority ethnic Armenians of Nagorno-Karabakh backed by Armenia, and the Republic of Azerbaijan. As the war progressed, Armenia and Azerbaijan, both former Republics of the Soviet Union, Soviet Republics, entangled themselves in protracted, undeclared mountain warfare in the mountainous heights of Karabakh as Azerbaijan attempted to curb the secessionist movement in Nagorno-Karabakh. The National Assembly (Nagorno-Karabakh), enclave's parliament had voted in favor of uniting with Armenia and a referendum, boycotted by the Azerbaijani population of Nagorno-Karabakh, was held, in which a majority voted in favor of independence. The demand to unify with Arme ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nagorno-Karabakh Defence Army
The Artsakh Defence Army ( hy, Արցախի Հանրապետության պաշտպանության բանակ, Artsakhi Hanrapetut’yan pashtpanut’yan banak) is the defence force of the breakaway Republic of Artsakh (Nagorno-Karabakh). Established in 1992, it united previously disorganized self-defence units which were formed in the early 1990s with the goal of protecting the ethnic Armenian population of Artsakh from attacks by Soviet and Azerbaijani armed forces. History Establishment The Artsakh Defence Army was founded on 9 May 1992. It created "its own central command and military structure distinct from the Armenian Army." Its founders included Robert Kocharyan (the former President of Armenia, he was the first commander-in-chief of the Army); Serzh Sargsyan (former Prime Minister and President of Armenia); Vazgen Sargsyan (Armenia's Defence Minister 1992–93, State Minister in Charge of defence 1993–95, Armenia's Prime Minister 1998–99); Monte Melkonian (re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Azerbaijan Soviet Socialist Republic
Azerbaijan ( az, Азәрбајҹан, Azərbaycan, italics=no), officially the Azerbaijan Soviet Socialist Republic (Azerbaijan SSR; az, Азәрбајҹан Совет Сосиалист Республикасы, Azərbaycan Sovet Sosialist Respublikası, italics=no, links=no; russian: Азербайджанская Советская Социалистическая Республика �зССРAzerbaydzhanskaya Sovetskaya Sotsialisticheskaya Respublika zSSR}), also referred to as Soviet Azerbaijan, was one of the constituent republics of the Soviet Union between 1922 and 1991. Created on 28 April 1920 when the Russian Soviet Federative Socialist Republic brought pro-Soviet figures to power in the region, the first two years of the Azerbaijani SSR were as an independent country until incorporation into the Transcausasian SFSR, along with the Armenian SSR and the Georgian SSR. In December 1922, the Transcaucasian SFSR became part of the newly established Soviet Union. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mausoleum In Mamedbeyli-IMG 8021
A mausoleum is an external free-standing building constructed as a monument enclosing the interment space or burial chamber of a deceased person or people. A mausoleum without the person's remains is called a cenotaph. A mausoleum may be considered a type of tomb, or the tomb may be considered to be within the mausoleum. Overview The word ''mausoleum'' (from Greek μαυσωλείον) derives from the Mausoleum at Halicarnassus (near modern-day Bodrum in Turkey), the grave of King Mausolus, the Persian satrap of Caria, whose large tomb was one of the Seven Wonders of the Ancient World. Historically, mausolea were, and still may be, large and impressive constructions for a deceased leader or other person of importance. However, smaller mausolea soon became popular with the gentry and nobility in many countries. In the Roman Empire, these were often in necropoles or along roadsides: the via Appia Antica retains the ruins of many private mausolea for kilometres outside Rome. Whe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals 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, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for lim ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gold
Gold is a chemical element with the symbol Au (from la, aurum) and atomic number 79. This makes it one of the higher atomic number elements that occur naturally. It is a bright, slightly orange-yellow, dense, soft, malleable, and ductile metal in a pure form. Chemically, gold is a transition metal and a group 11 element. It is one of the least reactive chemical elements and is solid under standard conditions. Gold often occurs in free elemental ( native state), as nuggets or grains, in rocks, veins, and alluvial deposits. It occurs in a solid solution series with the native element silver (as electrum), naturally alloyed with other metals like copper and palladium, and mineral inclusions such as within pyrite. Less commonly, it occurs in minerals as gold compounds, often with tellurium ( gold tellurides). Gold is resistant to most acids, though it does dissolve in aqua regia (a mixture of nitric acid and hydrochloric acid), forming a soluble tetrachloro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Molybdenum
Molybdenum is a chemical element with the symbol Mo and atomic number 42 which is located in period 5 and group 6. The name is from Neo-Latin ''molybdaenum'', which is based on Ancient Greek ', meaning lead, since its ores were confused with lead ores. Molybdenum minerals have been known throughout history, but the element was discovered (in the sense of differentiating it as a new entity from the mineral salts of other metals) in 1778 by Carl Wilhelm Scheele. The metal was first isolated in 1781 by Peter Jacob Hjelm. Molybdenum does not occur naturally as a free metal on Earth; it is found only in various oxidation states in minerals. The free element, a silvery metal with a grey cast, has the sixth-highest melting point of any element. It readily forms hard, stable carbides in alloys, and for this reason most of the world production of the element (about 80%) is used in steel alloys, including high-strength alloys and superalloys. Most molybdenum compounds have low solubility ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karabakh
Karabakh ( az, Qarabağ ; hy, Ղարաբաղ, Ġarabaġ ) is a geographic region in present-day southwestern Azerbaijan and eastern Armenia, extending from the highlands of the Lesser Caucasus down to the lowlands between the rivers Kura and Aras. It is conventionally divided into three regions: Highland Karabakh, Lowland Karabakh (the steppes between the Kura and Aras rivers), and the eastern slopes of the Zangezur Mountains (roughly Syunik and Kalbajar–Lachin). Hewsen, Robert H. "The Meliks of Eastern Armenia: A Preliminary Study," '' Revue des Études Arméniennes'' 9 (1972), p. 289, note 17. Etymology The Russian name , transliterated , derives from the Azerbaijani , which is generally believed to be a compound of the Turkic word ''kara'' (black) and the Iranian word ''bagh'' (garden), literally meaning "black garden." The Iranian Azerbaijanis, Iranian-Azerbaijani historian Ahmad Kasravi also speaks of the translation of ''kara'' as "large" and not "black." T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorga ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vorotan River
The Vorotan (), or Bargushad () or Bazarchay ( az, Bazarçay), is a river in Transcaucasia that is the largest right tributary of the Hakari river. The river originates in the mountains of Azerbaijan's Kalbajar District and flows into Armenia's Syunik Province. It flows through Armenia for in a generally south-easterly direction. The river enters Azerbaijan again, flowing for through the districts of Qubadli and Zangilan. The lower section of the Hakari, from its confluence with the Vorotan until its confluence with the Aras river, is sometimes considered to be part of the Vorotan. Course of the river The river flows mostly through mountainous country and in several places has formed deep canyons. The towns of Sisian and Qubadli lie along its course. Six kilometers from Sisian, the river forms a waterfall — the "Shaki Waterfall" ( hy, Շաքիի ջրվեժ) — that is 18m high. The river forms a natural monument — the "Devil's Bridge" — near Tatev Monastery. There are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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