Sian Lowland
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Sian Lowland
Sian Lowland or Oversian basin ( uk, Надсіанська котловина) is a lowland located at the border between Poland and Ukraine along the San River. Most of the region is located in Poland except for a small portion in southeastern end which is in Ukraine. The lowland is located between Malopolska Upland, Carpathian Foothills, Opillia Upland and Roztochia. To the southeast it extends into Dniester Lowland over the Sian-Dniester Divide. The Sian Lowland is a tectonic depression along the foothills of the Carpathian Mountains filled in by Miocene strata (up to thick) covered with glacial and alluvial deposits. It consists of elevated plateaus (the tallest being Tarnohorod) dissected by the valleys of rivers, such as the Tanew River, the Liubachivka River, the Shklo River, and the Vyshnia River. Loess can be found in parts of the plateaus, and dunes are situated in some of its sandy reaches. A large proportion of the lowland's forests have been cleared out, altho ...
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Poland
Poland, officially the Republic of Poland, is a country in Central Europe. It is divided into 16 administrative provinces called voivodeships, covering an area of . Poland has a population of over 38 million and is the fifth-most populous member state of the European Union. Warsaw is the nation's capital and largest metropolis. Other major cities include Kraków, Wrocław, Łódź, Poznań, Gdańsk, and Szczecin. Poland has a temperate transitional climate and its territory traverses the Central European Plain, extending from Baltic Sea in the north to Sudeten and Carpathian Mountains in the south. The longest Polish river is the Vistula, and Poland's highest point is Mount Rysy, situated in the Tatra mountain range of the Carpathians. The country is bordered by Lithuania and Russia to the northeast, Belarus and Ukraine to the east, Slovakia and the Czech Republic to the south, and Germany to the west. It also shares maritime boundaries with Denmark and Sweden. ...
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Glacial Deposit
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of '' glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is dep ...
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Plains Of Poland
In geography, a plain is a flat expanse of land that generally does not change much in elevation, and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or Highland, uplands. In a valley, a plain is enclosed on two sides, but in other cases a plain may be delineated by a complete or partial ring of hills, by mountains, or by cliffs. Where a geological region contains more than one plain, they may be connected by a Mountain pass, pass (sometimes termed a Gap (landform), gap). Coastal plains mostly rise from sea level until they run into elevated features such as mountains or plateaus. Plains are one of the major landforms on earth, where they are present on all continents, and cover more than one-third of the world's land area. Plains can be formed from flowing lava; from deposition of sediment by water, ice, or wind; or formed by erosion by the agents from hills and mountains. Biomes on plains include g ...
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Encyclopedia Of Ukraine
The ''Encyclopedia of Ukraine'' ( uk, Енциклопедія українознавства, translit=Entsyklopediia ukrainoznavstva), published from 1984 to 2001, is a fundamental work of Ukrainian Studies. Development The work was created under the auspices of the Shevchenko Scientific Society in Europe (Sarcelles, near Paris). As the ''Encyclopedia of Ukrainian Studies'' it conditionally consists of two parts, the first being a general part that consists of a three volume reference work divided in to subjects or themes. The second part is a 10 volume encyclopedia with entries arranged alphabetically. The editor-in-chief of Volumes I and II (published in 1984 and 1988 respectively) was Volodymyr Kubijovyč. The concluding three volumes, with Danylo Husar Struk as editor-in-chief, appeared in 1993. The encyclopedia set came with a 30-page ''Map & Gazetteer of Ukraine'' compiled by Kubijovyč and Arkadii Zhukovsky. It contained a detailed fold-out map (scale 1:2,000,000). ...
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Hornbeam
Hornbeams are hardwood trees in the flowering plant genus ''Carpinus'' in the birch family Betulaceae. The 30–40 species occur across much of the temperate regions of the Northern Hemisphere. Origin of names The common English name ''hornbeam'' derives from the hardness of the woods (likened to horn) and the Old English ''beam'' "tree" (cognate with Dutch ‘’Boom’’ and German ''Baum''). The American hornbeam is also occasionally known as blue-beech, ironwood, or musclewood, the first from the resemblance of the bark to that of the American beech ''Fagus grandifolia'', the other two from the hardness of the wood and the muscled appearance of the trunk and limbs. The botanical name for the genus, ''Carpinus'', is the original Latin name for the European species, although some etymologists derive it from the Celtic for a yoke. Taxonomy Formerly some taxonomists segregated them with the genera ''Corylus'' ( hazels) and ''Ostrya'' (hop-hornbeams) in a separate family, Coryl ...
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Loess
Loess (, ; from german: Löss ) is a clastic, predominantly silt-sized sediment that is formed by the accumulation of wind-blown dust. Ten percent of Earth's land area is covered by loess or similar deposits. Loess is a periglacial or aeolian (windborne) sediment, defined as an accumulation of 20% or less of clay and a balance of roughly equal parts sand and silt (with a typical grain size from 20 to 50 micrometers), often loosely cemented by calcium carbonate. It is usually homogeneous and highly porous and is traversed by vertical capillaries that permit the sediment to fracture and form vertical bluffs. Properties Loess is homogeneous, porous, friable, pale yellow or buff, slightly coherent, typically non- stratified and often calcareous. Loess grains are angular, with little polishing or rounding, and composed of crystals of quartz, feldspar, mica and other minerals. Loess can be described as a rich, dust-like soil. Loess deposits may become very thick, more than ...
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Shklo River
Shklo ( uk, Шкло, pl, Szkło) is an urban-type settlement in Yavoriv Raion, Lviv Oblast, in southwest Ukraine. It belongs to Novoiavorivsk urban hromada, one of the hromadas of Ukraine. Population: . Shklo is situated in the from the regional center Lviv, from the district center Yavoriv, and from Krakovets. Sanatorium treatment In the village located sanatorium “Shklo” He is rich in the unique combination of natural medicinal factors. There are drinkable sources of slightly mineralised water “Naftusia-Shklo”, hydrogen-sulphidous springs of high and middle mineralization and peaty-mineral medicinal muds. Culture The village has two sights of architecture Yavoriv district: * Church of St. Paraskeva (wooden) 1732 (1454 /1). * The bell tower of the church of St. Paraskeva (wooden) 1732 (1454 /2). And the village has one sight of architecture local importance: * The Parish School of the 18th century. (556–м). Personalities * Hordynsky Yaroslav Antonovic ...
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Tanew River
Tanew is a river in south-east Poland, a tributary of San. It starts in Roztocze hills. Tanew has a length of about 113 km and its catchment area is 2339 km². Its tributaries are: Potok Łosiniecki (R), Jeleń (R), Sopot (R), Szum (R), Łada (R), Wirowa (L), Lubienia (L), Złota Nitka Złota may refer to the following places: * Złota, Lesser Poland Voivodeship (south Poland) * Złota, Łódź Voivodeship (central Poland) *Złota, Pińczów County Złota is a village in Pińczów County, Świętokrzyskie Voivodeship, in south- ... (L), Łazowna (L), and Borowina (L). Rivers of Poland Rivers of Podkarpackie Voivodeship Rivers of Lublin Voivodeship {{Poland-river-stub ...
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Alluvial Deposit
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not Consolidation (geology), consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present Scientific consensus, consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman ...
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