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West Lusatian Hill Country And Uplands
The West Lusatian Hill Country and Uplands (german: Westlausitzer Hügel- und Bergland), sometimes just the West Lusatian Hills, at zip-code.en. Retrieved 12 Oct 2013 is a natural region in Saxony. It is divided into the West Lusatian Foothills (''Westlausitzer Vorberge'') in the east and the Lusatian Plateau (''Lausitzer Platte'') in the west and forms the westernmost extremity of the Sudetes range. Location and boundaries The West Lusatian Foothills form the northwestern declivity of the |
Ohorn Schwedenstein-Berg Mike Krüger 091203 1
Ohorn is a municipality in the district of Bautzen, in Saxony, Germany. Ohorn is a governmentally accredited recreation locality. Geography and infrastructure The municipality is located 2 km east of Pulsnitz and 30 km to the northeast of Dresden, the capital of Saxony. Embedded in the valley of the River Pulsnitz, Ohorn is surrounded by the typical landscape of the western Lusatian Hills, reaching a height of 449 m at the ''Hochstein'' Hill. Ohorn, having its own exit can be reached by using the A4 federal autobahn. Local subdivision Ohorn is divided into 5 parts: Fuchsbelle, Gickelsberg, Mitteldorf, Oberdorf and Röder. Historical development Following German Teutonic knights' call, in 1110 craftsmen, manufacturers and farmers from Thuringia, Franconia, Hesse and Bavaria came to settle in the area of the river Pulsnitz valley, creating a settlement of approximately on the southwestern side of the ''Schleißberg'' Hill, the river being an important factor in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Radeberg Land
Radeberg is a small town in the district of Bautzen, Saxony, Germany. It is located approximately 20 kilometres north-east of Dresden. The town has an Evangelical and a Roman Catholic church, and an old castle. History Radeberg was mentioned for the first time in 1219, when farmers settled on the country to the large Roeder. The name of the place is probably derived from this river. In less than 150 years a market place, a castle and own units developed. In the year 1412 the municipal law was lent to the small market town. 500 years ago silver was found close of the town. The discovery site was thereupon renamed as Silver Hill. The mine was however quickly exhausted. Industry Its principal industries are the manufacture of glass, machinery, furniture and paper, and it produces a light lager " Radeberger Beer" which is largely exported. The company ''Robotron Elektronik Radeberg'', formerly well known in East Germany for the production of portable television sets and powerful ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sand
Sand is a granular material composed of finely divided mineral particles. Sand has various compositions but is defined by its grain size. Sand grains are smaller than gravel and coarser than silt. Sand can also refer to a textural class of soil or soil type; i.e., a soil containing more than 85 percent sand-sized particles by mass. The composition of sand varies, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non-tropical coastal settings is silica (silicon dioxide, or SiO2), usually in the form of quartz. Calcium carbonate is the second most common type of sand, for example, aragonite, which has mostly been created, over the past 500million years, by various forms of life, like coral and shellfish. For example, it is the primary form of sand apparent in areas where reefs have dominated the ecosystem for millions of years like the Caribbean. Somewhat more rarely, sand may be composed of calciu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Syenite
Syenite is a coarse-grained intrusive igneous rock with a general composition similar to that of granite, but deficient in quartz, which, if present at all, occurs in relatively small concentrations (< 5%). Some syenites contain larger proportions of components and smaller amounts of felsic material than most granites; those are classed as being of . The equivalent of syenite is |
Greywacke
Greywacke or graywacke (German ''grauwacke'', signifying a grey, earthy rock) is a variety of sandstone generally characterized by its hardness, dark color, and poorly sorted angular grains of quartz, feldspar, and small rock fragments or lithic fragments set in a compact, clay-fine matrix. It is a texturally immature sedimentary rock generally found in Paleozoic strata. The larger grains can be sand- to gravel-sized, and matrix materials generally constitute more than 15% of the rock by volume. The term "greywacke" can be confusing, since it can refer to either the immature (rock fragment) aspect of the rock or its fine-grained (clay) component. The origin of greywacke was unknown until turbidity currents and turbidites were understood, since, according to the normal laws of sedimentation, gravel, sand and mud should not be laid down together. Geologists now attribute its formation to submarine avalanches or strong turbidity currents. These actions churn sediment and cause mi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lusatian Granite
Lusatian may refer to: * Lusatian languages (''Sorbian languages'') * Lusatians (people) (''Sorbs'') * Lusatia (''Sorbia'') * Lusatian culture The Lusatian culture existed in the later Bronze Age and early Iron Age (1700 BC – 500 BC) in most of what is now Poland and parts of the Czech Republic, Slovakia, eastern Germany and western Ukraine. It covers the Periods Montelius III (earl ..., of the later Bronze Age and early Iron Age {{disambig Language and nationality disambiguation pages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granodiorite
Granodiorite () is a coarse-grained (phaneritic) intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. The term banatite is sometimes used informally for various rocks ranging from granite to diorite, including granodiorite. Composition According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. A greater amount of plagioclase would designate the rock as tonalite. Granodiorite is felsic to intermediate in composition. It is the intrusive igneous equivalent of the extrusive igneous dacite. It contains a large amount of sodium (Na) and calcium (Ca) rich plagioclase, potassium feldspar, quartz, and minor amounts of muscovite mica as the lighter colored mineral components. Biotite and amphiboles often in the form of hornblende are more abundant in granodiorite than in granite, giving it a more distinct two-toned or overall darker appearan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rift
In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. Where rifts remain above sea level they form a rift valley, which may be filled by water forming a rift lake. The axis of the rift area may contain volcanic rocks, and active volcanism is a part of many, but not all, active rift systems. Major rifts occur along the central axis of most mid-ocean ridges, where new oceanic crust and lithosphere is created along a divergent boundary between two tectonic plates. ''Failed rifts'' are the result of continental rifting that failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a triple junction where three converging rifts meet over a hotspot. Two of these evolve to the poi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault-block
Fault blocks are very large blocks of rock, sometimes hundreds of kilometres in extent, created by tectonic and localized stresses in Earth's crust. Large areas of bedrock are broken up into blocks by faults. Blocks are characterized by relatively uniform lithology. The largest of these fault blocks are called crustal blocks. Large crustal blocks broken off from tectonic plates are called terranes. Those terranes which are the full thickness of the lithosphere are called microplates. Continent-sized blocks are called variously ''microcontinents, continental ribbons, H-blocks, extensional allochthons and outer highs.'' Because most stresses relate to the tectonic activity of moving plates, most motion between blocks is horizontal, that is parallel to the Earth's crust by strike-slip faults. However vertical movement of blocks produces much more dramatic results. Landforms (mountains, hills, ridges, lakes, valleys, etc.) are sometimes formed when the faults have a large ver ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dresden Elbe Slopes
Dresden (, ; Upper Saxon: ''Dräsdn''; wen, label=Upper Sorbian, Drježdźany) is the capital city of the German state of Saxony and its second most populous city, after Leipzig. It is the 12th most populous city of Germany, the fourth largest by area (after Berlin, Hamburg and Cologne), and the third most populous city in the area of former East Germany, after Berlin and Leipzig. Dresden's urban area comprises the towns of Freital, Pirna, Radebeul, Meissen, Coswig, Radeberg and Heidenau and has around 790,000 inhabitants. The Dresden metropolitan area has approximately 1.34 million inhabitants. Dresden is the second largest city on the River Elbe after Hamburg. Most of the city's population lives in the Elbe Valley, but a large, albeit very sparsely populated area of the city east of the Elbe lies in the West Lusatian Hill Country and Uplands (the westernmost part of the Sudetes) and thus in Lusatia. Many boroughs west of the Elbe lie in the foreland of the Ore Mountain ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schönfeld Upland
The Schönfeld Upland (german: Schönfelder Hochland) is a plateau in Dresden. It is named after Schönfeld, the district of Dresden in the middle of the plateau. Up to 1950, when Pillnitz was incorporated into Dresden, the upland was known as the Pillnitzer Elbe Plateau. Location The Schönfeld Upland is in the east of the Saxon capital of Dresden. It extends over an area of approximately 45 square kilometres to the edges of neighbouring Dürröhsdorf-Dittersbach in the rural district of Sächsische Schweiz-Osterzgebirge. Places in the Schönfeld Upland include Borsberg, Cunnersdorf, Eichbusch, Eschdorf, Gönnsdorf, Helfenberg, Krieschendorf, Malschendorf, Pappritz, Reitzendorf, Rockau, Rosinendörfchen, Rossendorf, Schönfeld, Schullwitz, Weißig and Zaschendorf. The Dresden districts of Rochwitz, Oberwachwitz (where the Dresden TV Tower is located) and Bühlau are also part of the landscape of the Schönfelder Upland. The Schönfeld Upland is part of the West ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
