Candy Cane Mountains
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Candy Cane Mountains
The Candy Cane Mountains ( az, Şəkər əsası dağları) are shale mountains in the Khizi and Siyazan districts of Azerbaijan, part of the Greater Caucasus mountain range. The 'Candy Cane Mountains' were originally dubbed so by travel author Mark Elliott in his guidebook 'Azerbaijan with Excursions to Georgia'. The mountains' colors are produced by groundwater that alters the oxidation state of the iron compounds in the earth. The Candy Cane Mountains contain numerous belemnites and fossils from the Cretaceous The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of th ... period, many of which can be spotted on the surface. See also * Orography of Azerbaijan References Mountains of Azerbaijan Khizi District Siyazan District Shale formations Tourist attractions in Azerbaijan ...
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Alti Agac
This is a list of significant characters from the television programs ''Hercules: The Legendary Journeys'', its prequel ''Young Hercules'', and '' Xena: Warrior Princess''. Main characters * Hercules (portrayed by Kevin Sorbo as an adult, Ian Bohen as young Hercules in flashbacks, Ryan Gosling as young Hercules in ''Young Hercules'') - The demi-god son of Zeus and Alcmene and strongest man in the world, and arch-rival to his older half brother Ares, the God of War. The champion of man who defeated and reformed the once power-hungry warlord Xena making her see the errors of her ways that set her on her path of redemption * Iolaus (portrayed by Michael Hurst as an adult, and Dean O'Gorman as young Iolaus in flashbacks and in ''Young Hercules'') - Hercules' sidekick, best friend, and companion. * Xena (portrayed by Lucy Lawless) - Once a power-hungry warlord, she was shown the error of her ways by Hercules and later repented and renounced her old life as an evil warrior. However, as ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ...
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Khizi District
Khizi District ( az, Xızı rayonu) is one of the 66 districts of Azerbaijan. It is located in the east of the country and belongs to the Absheron-Khizi Economic Region. The district borders the districts of Siyazan, Shabran, Quba, Shamakhi, Gobustan, and Absheron-Khizi. Its capital and largest city is Khizi. As of 2020, the district had a population of 17,100, making it the least populated district of Azerbaijan. Etymology Azerbaijanis and Tats compose the main ethnic background of Khizi. There are preconceptions about the etymology of the word "Xızı" which was previously used to represent a small village. Many experts assume that this name is from the Sassanid Empire. In the early Middle Ages (III-VI centuries), the Iranian tribes were transferred here to spread the Zoroastrianism, the official religion of the Empire, in northern territories of the empire, to combat Christianity and protect the northern borders from Hun, Peach and Khazar tribes. This process further st ...
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Siyazan District
Siyazan District ( az, Siyəzən rayonu) is one of the 66 districts of Azerbaijan. It is located in the north-east of the country and belongs to the Guba-Khachmaz Economic Region. The district borders the districts of Shabran, Khizi, and the exclaves of Quba. Its capital and largest city is Siyazan. As of 2020, the district had a population of 42,600. Etymology The name is believed to be derived from Persian, meaning "White Women", a reference to the original inhabitants, Tats. Another theory links the name with the Persian word ''siyah'', meaning "black". History The villages of Agh Siyazan ("White Siyazan") and Gara Siyazan ("Black Siyazan") formerly existed in the territory of the Siyazan District and the city was formerly called ''Gizilburun'' ( az, Qızılburun). When the Baku-Shollar Pipeline was being constructed between 1911 and 1916, people started moving in from the surrounding villages as a labour force. The "Gizilburun" railway station also played a role in the tr ...
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Azerbaijan
Azerbaijan (, ; az, Azərbaycan ), officially the Republic of Azerbaijan, , also sometimes officially called the Azerbaijan Republic is a transcontinental country located at the boundary of Eastern Europe and Western Asia. It is a part of the South Caucasus region and is bounded by the Caspian Sea to the east, Russia (Republic of Dagestan) to the north, Georgia to the northwest, Armenia and Turkey to the west, and Iran to the south. Baku is the capital and largest city. The Azerbaijan Democratic Republic proclaimed its independence from the Transcaucasian Democratic Federative Republic in 1918 and became the first secular democratic Muslim-majority state. In 1920, the country was incorporated into the Soviet Union as the Azerbaijan SSR. The modern Republic of Azerbaijan proclaimed its independence on 30 August 1991, shortly before the dissolution of the Soviet Union in the same year. In September 1991, the ethnic Armenian majority of the Nagorno-Karabakh region formed the ...
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Greater Caucasus
The Greater Caucasus ( az, Böyük Qafqaz, Бөјүк Гафгаз, بيوک قافقاز; ka, დიდი კავკასიონი, ''Didi K’avk’asioni''; russian: Большой Кавказ, ''Bolshoy Kavkaz'', sometimes translated as "''Caucasus Major''", "''Big Caucasus''" or "''Large Caucasus''") is the major mountain range of the Caucasus Mountains. The range stretches for about from west-northwest to east-southeast, between the Taman Peninsula of the Black Sea to the Absheron Peninsula of the Caspian Sea: from the Western Caucasus in the vicinity of Sochi on the northeastern shore of the Black Sea and reaching nearly to Baku on the Caspian. Geography The range is traditionally separated into three parts: * The Western Caucasus, between the Black Sea and Mount Elbrus * The Central Caucasus, between Mount Elbrus and Mount Kazbek * The Eastern Caucasus, between Mount Kazbek and the Caspian Sea In the wetter Western Caucasus, the mountains are heavily forest ...
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Mark Elliott (British Author)
Mark Elliott is an English travel writer best known for books on Azerbaijan, and for unusual map-based route guides for Asia. Though long out of print, Elliott's ''Asia Overland'' co-authored with Wil Klass, garnered something of a cult following among overland travellers during the late 1990s. Elliott's 2003 ''South-East Asia: The Graphic Guide'', also based mostly on schematic maps, remains in considerable demand among travellers with prices for second hand copies reaching absurdly high levels (nearly US$1000 a copy in November 2009). He also contributed to over 50 Lonely Planet guides. Having written the first comprehensive English language guide to post-Soviet Azerbaijan in 1999, a book now in its 5th edition, Elliott has since been described by the press in Azerbaijan as the "legendary writer of the definitive English-language guidebook to the country" Early life Elliott's father Ian was the chairman of West Sussex County Council, his mother the teacher and poet, Betty Ell ...
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Groundwater
Groundwater is the water present beneath Earth's surface in rock and soil pore spaces and in the fractures of rock formations. About 30 percent of all readily available freshwater in the world is groundwater. A unit of rock or an unconsolidated deposit is called an aquifer when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the water table. Groundwater is recharged from the surface; it may discharge from the surface naturally at springs and seeps, and can form oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction wells. The study of the distribution and movement of groundwater is hydrogeology, also called groundwater hydrology. Typically, groundwater is thought of as water flowing through shallow aquifers, but, in the technical sense, it can also contain soil moisture, perma ...
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Oxidation State
In chemistry, the oxidation state, or oxidation number, is the hypothetical charge of an atom if all of its bonds to different atoms were fully ionic. It describes the degree of oxidation (loss of electrons) of an atom in a chemical compound. Conceptually, the oxidation state may be positive, negative or zero. While fully ionic bonds are not found in nature, many bonds exhibit strong ionicity, making oxidation state a useful predictor of charge. The oxidation state of an atom does not represent the "real" formal charge on that atom, or any other actual atomic property. This is particularly true of high oxidation states, where the ionization energy required to produce a multiply positive ion is far greater than the energies available in chemical reactions. Additionally, the oxidation states of atoms in a given compound may vary depending on the choice of electronegativity scale used in their calculation. Thus, the oxidation state of an atom in a compound is purely a formalism. ...
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Iron
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or furnaces capable of reaching or higher, about higher than that required to smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BCE and the use of iron tools and weapons began to displace copper alloys, in some regions, only around 1200 BCE. That event is considered the transition from the Bronze Age to the Iron A ...
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OSCE
The Organization for Security and Co-operation in Europe (OSCE) is the world's largest regional security-oriented intergovernmental organization with observer status at the United Nations. Its mandate includes issues such as arms control, promotion of human rights, freedom of the press, and free and fair elections. It employs around 3,460 people, mostly in its field operations but also in its secretariat in Vienna, Austria, and its institutions. It has its origins in the mid-1975 Conference on Security and Co-operation in Europe (CSCE) held in Helsinki, Finland. The OSCE is concerned with early warning, conflict prevention, crisis management, and post-conflict rehabilitation. Most of its 57 participating countries are in Europe, but there are a few members present in Asia and North America. The participating states cover much of the land area of the Northern Hemisphere. It was created during the Cold War era as a forum for discussion between the Western Bloc and Eastern Bl ...
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Belemnite
Belemnitida (or the belemnite) is an extinct order of squid-like cephalopods that existed from the Late Triassic to Late Cretaceous. Unlike squid, belemnites had an internal skeleton that made up the cone. The parts are, from the arms-most to the tip: the tongue-shaped pro-ostracum, the conical phragmocone, and the pointy guard. The calcitic guard is the most common belemnite remain. Belemnites, in life, are thought to have had 10 hooked arms and a pair of fins on the guard. The chitinous hooks were usually no bigger than , though a belemnite could have had between 100 and 800 hooks in total, using them to stab and hold onto prey. Belemnites were an important food source for many Mesozoic marine creatures, both the adults and the planktonic juveniles, and likely played an important role in restructuring marine ecosystems after the Triassic–Jurassic extinction event. They may have laid between 100 and 1,000 eggs. Some species may have been adapted to speed and swam in the tur ...
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