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Meiselberg
The Meiselberg is a hill in the 19th district of Vienna, Döbling. It is 291 metres tall Geography The Meiselberg represents the north-eastern extension of the Schenkenberg and lies in the suburb of Sievering. The limits of the Meiselberg are defined by the Kaasgraben to the north and the Arbesbach to the south. The hill is part of a north-eastern chain of foothills belonging to the eastern Alps. It is composed of flysch containing quartz, limestone, marl, and other conglomerates. History The name Meiselberg is probably a reference to the hill's steep ridge and most likely derives from the Middle High German ''meizel'' (meaning chisel). Today, the hill is sparsely settled, but in contrast to the surrounding hills, is not used for viticulture Viticulture (from the Latin word for ''vine'') or winegrowing (wine growing) is the cultivation and harvesting of grapes. It is a branch of the science of horticulture. While the native territory of ''Vitis vinifera'', the common grap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sievering
Sievering is a suburb of Vienna and part of Döbling, the 19th district of Vienna. Sievering was created in 1892 out of the two erstwhile independent suburbs Untersievering and Obersievering. These still exist as Katastralgemeinden. For many years it was home to the Sievering Studios, one of Austria's leading film studios. Geography Sievering arose on the banks of the Arbesbach, Vienna, Arbesbach. The more modern distinction between Obersievering and Untersievering coincides with the route of this stream; Obersievering (Upper Sievering) lies between the Schenkenberg, Vienna, Schenkenberg and Hackenberg, Vienna, Hackenberg and therefore upstream of Untersievering (Lower Sievering), which lies to the south of the Meiselberg. An abandoned village named Mitterhofen once lay between the two Sieverings. It was the earliest settlement, consisting of a group of houses around a chapel, but it was subsumed by the towns to either side of it. Chlaintzing, another village which stood on t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vienna
en, Viennese , iso_code = AT-9 , registration_plate = W , postal_code_type = Postal code , postal_code = , timezone = CET , utc_offset = +1 , timezone_DST = CEST , utc_offset_DST = +2 , blank_name = Vehicle registration , blank_info = W , blank1_name = GDP , blank1_info = € 96.5 billion (2020) , blank2_name = GDP per capita , blank2_info = € 50,400 (2020) , blank_name_sec1 = HDI (2019) , blank_info_sec1 = 0.947 · 1st of 9 , blank3_name = Seats in the Federal Council , blank3_info = , blank_name_sec2 = GeoTLD , blank_info_sec2 = .wien , website = , footnotes = , image_blank_emblem = Wien logo.svg , blank_emblem_size = Vienna ( ; german: Wien ; ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Döbling
Döbling () is the 19th District A district is a type of administrative division that, in some countries, is managed by the local government. Across the world, areas known as "districts" vary greatly in size, spanning regions or counties, several municipalities, subdivisions o ... in the city of Vienna, Austria (german: 19. Bezirk, Döbling, Doebling). It is located on the north end from the central districts, north of the districts Alsergrund and Währing. Döbling has some heavily populated urban areas with many residential buildings, and borders the Vienna Woods. Statistik Austria, 2008, website: (in German: population is "Einwohner"). Wien.gv.at webpage (see below: References). It hosts some of the most expensive residential areas such as Grinzing, Sievering, Neustift am Walde and Kaasgraben and is also the site of many ''Heurigen'' restaurants. There are also some large ''Gemeindebauten'', including Vienna's most famous, the Karl-Marx-Hof. Also located in Döbling is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schenkenberg, Vienna
The Schenkenberg is a hill in the 19th district of Vienna, Döbling. It is 345 metres tall. Geography The Schenkenberg lies in Obersievering and represents the south-eastern extension of the Pfaffenberg. To the north, the Reisenbergbach separates the Schenkenberg from the Reisenberg; to the south, the Arbesbach divides it from the Hackenberg. The Schenkenberg is part of a north-eastern chain of foothills belonging to the eastern Alps. It is composed of flysch containing quartz, limestone, marl, and other conglomerates. History The first documentary reference to the Schenkenberg dates from 1329 and dubs it ''in dem Schenkenberge''. The name Schenkenberg is probably a reference to the Mundschenk family, which owned land in the area. The Kuenringer, who also owned property in this area, were called the ''Oberste Schenken''. Today, the Schenkenberg is surrounded by numerous vineyards A vineyard (; also ) is a plantation of grape-bearing vines, grown mainly for winema ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arbesbach, Vienna
The Arbesbach, also known as the ''Erbsenbach'' and ''Sieveringerbach'', is a stream in Döbling, the 19th district of Vienna, Austria. The stream, partially enclosed in a canal, is the most important tributary of the . Almost all of its lie within the suburb of Sievering. Geography Geology The Arbesbach, which makes its way through the Vienna Woods, is characteristic for streams in low mountainous areas (). Because the ground does not absorb much rainfall, the level of water in the stream can change rapidly when it rains heavily, resulting in flash flooding. The Arbesbach rises in the woods and runs over relatively steep ground that has been heavily eroded. Course Headwaters Several springs in the area between the and the flow together to form the headwaters of the Arbesbach. The most northerly springs rise to the south of the Jägerwiese and between the Latisberg and . These meet to the north of the Hartgrabenwiese and are quickly joined by another three springs, w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Alps
Eastern Alps is the name given to the eastern half of the Alps, usually defined as the area east of a line from Lake Constance and the Alpine Rhine valley up to the Splügen Pass at the Alpine divide and down the Liro River to Lake Como in the south. The peaks and mountain passes are lower than the Western Alps, while the range itself is broader and less arched. Geography Overview The Eastern Alps include the eastern parts of Switzerland (mainly Graubünden), all of Liechtenstein, and most of Austria from Vorarlberg to the east, as well as parts of extreme Southern Germany (Upper Bavaria), northwestern Italy (Lombardy), northeastern Italy (Trentino-Alto Adige/Südtirol, Veneto and Friuli-Venezia Giulia) and a good portion of northern Slovenia (Upper Carniola and Lower Styria). In the south the range is bound by the Italian Padan Plain; in the north the valley of the Danube River separates it from the Bohemian Massif. The easternmost spur is formed by the Vienna Woods range, wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flysch
Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians. Sedimentological properties Flysch consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard, graywacke-like sandstones. Typically the shales do not contain many fossils, while the coarser sandstones often have fractions of micas and glauconite. Tectonics In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartz
Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar. Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at . Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold. There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia. Quartz is the mineral defining the val ... [...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 limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. The te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
