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Ludogorie Plateau
The Ludogorie ( bg, Лудогорие, usually used with a definite article, Лудогорието, ''Ludogorieto'') or Deliorman (''Делиорман'', tr, Deli Orman, lit=mad forest and Bulgarian: lud - "mad", "crazy" and gora - "forest"), is a region in northeastern Bulgaria stretching over the plateau of the same name. Major cities in the region are Targovishte, Razgrad, Dulovo, Novi Pazar, Pliska, Preslav and Isperih. Part of the Danubian Plain, the region is hilly in the east, reaching up to in height near the village of Samuil, but merges with the plains of Dobruja and the Danube to the north, with the lowest point near Yuper (). The region is bordered to the west by the Provadiya River and the Beli Lom; to the east it transitions into the Dobruja plateau. The plateau was formed of Karst limestone from the Lower Cretaceous covered by loess material. Among the region's geological resources are kaolinite, fireclay and mica. The climate is temperate continental, with ...
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Ludogorie Sunset Iz2
The Ludogorie ( bg, Лудогорие, usually used with a definite article, Лудогорието, ''Ludogorieto'') or Deliorman (''Делиорман'', tr, Deli Orman, lit=mad forest and Bulgarian: lud - "mad", "crazy" and gora - "forest"), is a region in northeastern Bulgaria stretching over the plateau of the same name. Major cities in the region are Targovishte, Razgrad, Dulovo, Novi Pazar, Pliska, Preslav and Isperih. Part of the Danubian Plain, the region is hilly in the east, reaching up to in height near the village of Samuil, but merges with the plains of Dobruja and the Danube to the north, with the lowest point near Yuper (). The region is bordered to the west by the Provadiya River and the Beli Lom; to the east it transitions into the Dobruja plateau. The plateau was formed of Karst limestone from the Lower Cretaceous covered by loess material. Among the region's geological resources are kaolinite, fireclay and mica. The climate is temperate continental, with ...
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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 limes ...
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Balkan Mountains
The Balkan mountain range (, , known locally also as Stara planina) is a mountain range in the eastern part of the Balkan Peninsula in Southeastern Europe. The range is conventionally taken to begin at the peak of Vrashka Chuka on the border between Bulgaria and Serbia. It then runs for about , first in a south-easterly direction along the border, then eastward across Bulgaria, forming a natural barrier between the northern and southern halves of the country, before finally reaching the Black Sea at Cape Emine. The mountains reach their highest point with Botev Peak at . In much of the central and eastern sections, the summit forms the watershed between the drainage basins of the Black Sea and the Aegean. A prominent gap in the mountains is formed by the sometimes narrow Iskar Gorge, a few miles north of the Bulgarian capital, Sofia. The karst relief determines the large number of caves, including Magura, featuring the most important and extended European post-Palaeolithic cave ...
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World Heritage Site
A World Heritage Site is a landmark or area with legal protection by an international convention administered by the United Nations Educational, Scientific and Cultural Organization (UNESCO). World Heritage Sites are designated by UNESCO for having cultural, historical, scientific or other form of significance. The sites are judged to contain " cultural and natural heritage around the world considered to be of outstanding value to humanity". To be selected, a World Heritage Site must be a somehow unique landmark which is geographically and historically identifiable and has special cultural or physical significance. For example, World Heritage Sites might be ancient ruins or historical structures, buildings, cities, deserts, forests, islands, lakes, monuments, mountains, or wilderness areas. A World Heritage Site may signify a remarkable accomplishment of humanity, and serve as evidence of our intellectual history on the planet, or it might be a place of great natural beauty. A ...
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UNESCO
The United Nations Educational, Scientific and Cultural Organization is a specialized agency of the United Nations (UN) aimed at promoting world peace and security through international cooperation in education, arts, sciences and culture. It has 193 member states and 12 associate members, as well as partners in the non-governmental, intergovernmental and private sector. Headquartered at the World Heritage Centre in Paris, France, UNESCO has 53 regional field offices and 199 national commissions that facilitate its global mandate. UNESCO was founded in 1945 as the successor to the League of Nations's International Committee on Intellectual Cooperation.English summary). Its constitution establishes the agency's goals, governing structure, and operating framework. UNESCO's founding mission, which was shaped by the Second World War, is to advance peace, sustainable development and human rights by facilitating collaboration and dialogue among nations. It pursues this objective t ...
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Thracian Tomb Of Sveshtari
The Thracian Tomb of Svestari (Свещарска гробница, ''Sveshtarska grobnitsa'') is 2.5 km southwest of the village of Sveshtari, Razgrad Province, which is 42 km northeast of Razgrad, in northeast Bulgaria. The tomb is probably the grave of Dromichaetes ( grc, Δρομιχαίτης, Dromichaites; c. 300 – c. 280 BC) who was a king of the Getae on both sides of the lower Danube (present day Romania and Bulgaria) around 300 BC, and his wife, the daughter of King Lysimachus (Greek: Λυσίμαχος, ''Lysimachos''; c. 360 BC – 281 BC) who was a general and ''diadochus'' (i.e. "successor") of Alexander the Great. The tomb is a UNESCO World Heritage Site. General information Discovered and excavated in 1982 during excavations at Mound No 7 of the East Mound Necropolis of Sboryanovo (''Ginina Mogila'') - a tumulus of the early Hellenistic period, the Sveshtari tomb was built in the first quarter of the 3rd century BC. The tomb's construction reflects ...
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Getae
The Getae ( ) or Gets ( ; grc, Γέται, singular ) were a Thracian-related tribe that once inhabited the regions to either side of the Lower Danube, in what is today northern Bulgaria and southern Romania. Both the singular form ''Get'' and plural ''Getae'' may be derived from a Greek exonym: the area was the hinterland of Greek colonies on the Black Sea coast, bringing the Getae into contact with the ancient Greeks from an early date. Although it is believed that the Getae were related to their westward neighbours, the Dacians, several scholars, especially in the Romanian historiography, posit that the Getae and the Dacians were the same people. Ethnonym The ethnonym ''Getae'' was first used by Herodotus. The root was also used for the Tyragetae, Thyssagetae, Massagetae, and others. Getae and Dacians Ancient sources Strabo, one of the first ancient sources to mention Getae and Dacians, stated in his ''Geographica'' ( 7BC – 20AD) that the Dacians lived in the wes ...
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Thracians
The Thracians (; grc, Θρᾷκες ''Thrāikes''; la, Thraci) were an Indo-European languages, Indo-European speaking people who inhabited large parts of Eastern Europe, Eastern and Southeast Europe, Southeastern Europe in ancient history.. "The Thracians were an Indo-European people who occupied the area between northern Greece, southern Russia, and north-western Turkey. They shared the same language and culture... There may have been as many as a million Thracians, diveded among up to 40 tribes." Thracians resided mainly in the Balkans (mostly Present (time), modern day Bulgaria, Turkey and Greece) but were also located in Anatolia, Anatolia (Asia Minor) and other locations in Eastern Europe. The exact origin of Thracians is unknown, but it is believed that proto-Thracians descended from a purported mixture of Proto-Indo-Europeans and Early European Farmers, arriving from the rest of Asia and Africa through the Asia Minor (Anatolia). The proto-Thracian culture developed int ...
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Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condense ...
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Continental Climate
Continental climates often have a significant annual variation in temperature (warm summers and cold winters). They tend to occur in the middle latitudes (40 to 55 north), within large landmasses where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans. Continental climates occur mostly in the Northern Hemisphere due to the large landmasses found there. Most of northern and northeastern China, eastern and southeastern Europe, Western and north western Iran, central and southeastern Canada, and the central and northeastern United States have this type of climate. Continentality is a measure of the degree to which a region experiences this type of climate. In continental climates, precipitation tends to be moderate in amount, concentrated mostly in the warmer months. Only a few areas—in the mountains of the Pacific Northwest of North America and in Iran, northern Iraq, adjacent Turkey, Afghanistan, Pakistan, and Central Asia ...
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Mica
Micas ( ) are a group of silicate minerals whose outstanding physical characteristic is that individual mica crystals can easily be split into extremely thin elastic plates. This characteristic is described as perfect basal cleavage. Mica is common in igneous and metamorphic rock and is occasionally found as small flakes in sedimentary rock. It is particularly prominent in many granites, pegmatites, and schists, and "books" (large individual crystals) of mica several feet across have been found in some pegmatites. Micas are used in products such as drywalls, paints, fillers, especially in parts for automobiles, roofing and shingles, as well as in electronics. The mineral is used in cosmetics and food to add "shimmer" or "frost." Properties and structure The mica group is composed of 37 phyllosilicate minerals. All crystallize in the monoclinic system, with a tendency towards pseudohexagonal crystals, and are similar in structure but vary in chemical composition. Micas are ...
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Fireclay
Fire clay is a range of refractory clays used in the manufacture of ceramics, especially fire brick. The United States Environmental Protection Agency defines fire clay very generally as a "mineral aggregate composed of hydrous silicates of aluminium (Al2O3·2SiO2·2H2O) with or without free silica." Properties High-grade fire clays can withstand temperatures of 1,775 °C (3,227 °F), but to be referred to as a "fire clay" the material must withstand a minimum temperature of .Minerals Zone, World Mineral Exchange.
Retrieved 2011-6-23.
Fire clays range from ''s'' to ''plastic fire clays'', but there are ''semi-flint'' and ''semi-plastic'' fire clays as well. Fire clays consist ...
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