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Villmar Luftbild 062
Villmar is a market village and municipality in the Limburg-Weilburg district in Hesse, Germany. The community is the centre for quarrying and processing the so-called Lahn Marble. Geography Location Villmar lies in the Lahn River valley between the Westerwald and the Taunus, some ten kilometres east of Limburg. In terms of the natural environment, the southwestern part of the municipal area comprises the eastern part of the Limburg Basin (this part known locally as the Villmar Bay or ''Villmarer Bucht''), a nearly even two- to three-kilometre-wide plain that opens to the west lying at elevations of 160 to 180 m into which the Lahn's winding lower valley has cut a channel about 50 metres deep. Conditioned by the mild climate and the extensive loess soils, intensive crop production prevails here. To the north, the somewhat higher (220–260 m), more richly wooded ''Weilburger Lahntalgebiet'' ("Weilburg Lahn valley area") joins up with the ''Weilburger Lahntal'' ("Weilb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hessisches Statistisches Landesamt ...
The statistical offices of the German states (German: ''Statistische Landesämter'') carry out the task of collecting official statistics in Germany together and in cooperation with the Federal Statistical Office. The implementation of statistics according to Article 83 of the constitution is executed at state level. The federal government has, under Article 73 (1) 11. of the constitution, the exclusive legislation for the "statistics for federal purposes." There are 14 statistical offices for the 16 states: See also * Federal Statistical Office of Germany References {{Reflist Germany Statistical offices Germany Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated betwe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iron Ore
Iron ores are rocks and minerals from which metallic iron can be economically extracted. The ores are usually rich in iron oxides and vary in color from dark grey, bright yellow, or deep purple to rusty red. The iron is usually found in the form of magnetite (, 72.4% Fe), hematite (, 69.9% Fe), goethite (, 62.9% Fe), limonite (, 55% Fe) or siderite (, 48.2% Fe). Ores containing very high quantities of hematite or magnetite (greater than about 60% iron) are known as "natural ore" or "direct shipping ore", meaning they can be fed directly into iron-making blast furnaces. Iron ore is the raw material used to make pig iron, which is one of the main raw materials to make steel—98% of the mined iron ore is used to make steel. In 2011 the ''Financial Times'' quoted Christopher LaFemina, mining analyst at Barclays Capital, saying that iron ore is "more integral to the global economy than any other commodity, except perhaps oil". Sources Metallic iron is virtually unknown on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ortsteil
A village is a clustered human settlement or Residential community, community, larger than a hamlet (place), hamlet but smaller than a town (although the word is often used to describe both hamlets and smaller towns), with a population typically ranging from a few hundred to a few thousand. Though villages are often located in rural areas, the term urban village is also applied to certain urban neighborhoods. Villages are normally permanent, with fixed dwellings; however, transient villages can occur. Further, the dwellings of a village are fairly close to one another, not scattered broadly over the landscape, as a dispersed settlement. In the past, villages were a usual form of community for societies that practice subsistence agriculture, and also for some non-agricultural societies. In Great Britain, a hamlet earned the right to be called a village when it built a Church (building), church. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brechen
Brechen is a municipality in Limburg-Weilburg district in Hesse, Germany. Geography Location Brechen lies in the southeastern part of the Limburg Basin between the Taunus and the Westerwald. The sparsely wooded land of loess hills is crossed here from southeast to northwest by the Emsbach, which is fed near Niederbrechen by the Wörsbach and drains the area down to the Lahn. Together with the ''Idsteiner Senke'' (basin), which joins it in the south, this patch of countryside is customarily known as the ''Goldener Grund'' (“Golden Ground”), a reference to the favourable climate and the fruitful earth. Neighbouring communities In the northwest the community of Brechen borders on the district seat of Limburg, in the north on the town of Runkel, in the northeast on the market town of Villmar, in the southeast on the community of Selters and in the southwest on the community of Hünfelden (all in Limburg-Weilburg). Constituent communities Brechen's three ''Ortsteile'' are Nied ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Selters (Taunus)
Selters (Taunus) is a municipality with 8,000 inhabitants north of Bad Camberg in Limburg-Weilburg district in Hesse, Germany. Geography Location The greater part of the Selters municipal area with the centres of Niederselters, Eisenbach, Münster and Haintchen lies in the area of the Eastern Hintertaunus north of the Taunus' main ridge, at elevations from 170 to 500 m. In terms of natural environments, the main centre, Niederselters, also belongs to the southeastern part of the Limburg Basin. giving it a connection to the valley landscape of the Lahn. The fracture zone opening here into the basin from the south, the ''Idsteiner Senke'' (hollow), is locally known along the Emsbach, which empties into the Lahn, by the name ''Goldener Grund'' (“Golden Ground”), a reference to the favourable climate and fruitful soil (loess). The northern part of the community around Münster belongs geologically to the Lahn Basin, which is known for its mineral wealth from the Middle De ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weilmünster
Weilmünster is a municipality in Limburg-Weilburg district in Hesse, Germany. Geography Weilmünster is among the most richly wooded places in Limburg-Weilburg. The forestry office looks after not only the State Forest but also twelve municipalities’ woodlands in the south of the Limburg-Weilburg and Lahn-Dill districts. Location The market community of Weilmünster lies on the north slope of the Taunus in the Weil valley, the Weil being a tributary to the Lahn. The nearest major cities are Wetzlar (20 km) to the northeast, Limburg (25 km) to the west and Frankfurt am Main (50 km) to the southeast. Neighbouring communities Weilmünster borders in the north on the towns of Weilburg (Limburg-Weilburg) and Braunfels, in the east on the community of Waldsolms (both in the Lahn-Dill-Kreis), in the south on the communities of Grävenwiesbach, Weilrod (both in the Hochtaunuskreis) and Selters and in the west on the communities of Villmar and Weinbach (all thr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Weinbach
Weinbach is a municipality in Limburg-Weilburg district in Hesse, Germany. Geography Location Weinbach lies on the Lahn and the Weil between Wetzlar and Limburg an der Lahn. Neighbouring communities Weinbach borders in the north on the town of Weilburg, in the east on the community of Weilmünster, and in the west on the community of Villmar and the town of Runkel (all in Limburg-Weilburg). Constituent communities Weinbach is made up of eight ''Ortsteile''. The main centre is also called Weinbach, and the outlying centres are Blessenbach, Edelsberg, Elkerhausen, Freienfels, Fürfurt, Gräveneck and Kleinweinbach. History Fürfurt was mentioned in a document from sometime between 1148 and 1154, thus making it the first part of the community to have its first documentary mention. Elkerhausen’s first documentary mention came in 1191. The knightly family who lived there was heavily involved in a feud in the 14th century with the landlord, the Archbishop of Trier. The '' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Runkel
Runkel is a town on the river Lahn in Limburg-Weilburg district in Hesse, Germany. Geography Location Runkel lies in the Lahn Valley on both sides of the river between the Westerwald and the Taunus, some eight kilometres east of Limburg an der Lahn, Limburg. Neighbouring communities Runkel borders in the north on the community of Beselich and the town of Weilburg, in the east on the communities of Weinbach and Villmar and in the south and west on the town of Limburg. Constituent communities The town consists of 9 ''Stadtteile''. History The town's first documentary mention came in 1159 in an ''enfeoffment'' document in which a nobleman named Siegfried von Runkel had his name appear as a witness. It is believed that this Siegfried was the one who built Runkel Castle. In 1191 Siegfried married a countess of Katzenelnbogen. This high noble family forced Dietrich of Runkel to open his castles Runkel and Dehrn. No later than 1230, the castle had a chapel, thereby givi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanism
Volcanism, vulcanism or volcanicity is the phenomenon of eruption of molten rock (magma) onto the surface of the Earth or a solid-surface planet or moon, where lava, pyroclastics, and volcanic gases erupt through a break in the surface called a vent. It includes all phenomena resulting from and causing magma within the crust or mantle of the body, to rise through the crust and form volcanic rocks on the surface. Magmas, that reach the surface and solidify, form extrusive landforms. Volcanic processes Magma from the mantle or lower crust rises through the crust towards the surface. If magma reaches the surface, its behavior depends on the viscosity of the molten constituent rock. Viscous (thick) magma produces volcanoes characterised by explosive eruptions, while non-viscous (runny) magma produce volcanoes characterised by effusive eruptions pouring large amounts of lava onto the surface. In some cases, rising magma can cool and solidify without reaching the surface. Inste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tertiary
Tertiary ( ) is a widely used but obsolete term for the geologic period from 66 million to 2.6 million years ago. The period began with the demise of the non-avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene Epoch. The time span covered by the Tertiary has no exact equivalent in the current geologic time system, but it is essentially the merged Paleogene and Neogene periods, which are informally called the Early Tertiary and the Late Tertiary, respectively. The Tertiary established the Antarctic as an icy island continent. Historical use of the term The term Tertiary was first used by Giovanni Arduino during the mid-18th century. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of geology in Northern Italy. Later a fourth period, the Quaternary, was applied. In the early d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
