|
Limburg Basin
The Limburg Basin (german: Limburger Becken) is one of the two large intramontane lowland areas within the Rhenish Massif in Germany, the other being the Middle Rhine Basin. It forms the central part of the natural region of the Gießen-Koblenz Lahn Valley between the Weilburg Lahn Valley Region and the Lower Lahn Valley on both sides of the Lahn around the town of Limburg. Description The Limburg basin, which measures about 20 by 14 kilometres across and is almost treeless, is a tectonic intrusion field (''Einbruchsfeld'') and connects the more deeply incised valley sections in the Weilburg Lahn Valley area with those of the Lower Lahn Valley. It is divided into the North and South Limburg Basin Hills and the almost level Inner Limburg Basin, including the Villmar Bay and Linter Plateau, in whose bottom the winding course of the course of the Lahn has sunk about 50 metres deep. The hills that rise at the edges of the basin or within it form landmarks that are visible fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taunus - Deutsche Mittelgebirge, Serie A-de
The Taunus is a mountain range in Hesse, Germany, located north of Frankfurt. The tallest peak in the range is ''Großer Feldberg'' at 878 m; other notable peaks are ''Kleiner Feldberg'' (825 m) and ''Altkönig'' (798 m). The Taunus range spans the districts of Hochtaunuskreis, Main-Taunus-Kreis, Rheingau-Taunus, Limburg-Weilburg, and Rhein-Lahn. The range is known for its geothermal springs and mineral waters that formerly attracted members of the European aristocracy to its spa towns. The car line Ford Taunus is named after it. Description It is a relatively low range, with smooth, rounded mountains covered with forest. The Taunus is bounded by the valleys of the Rhine, Main, and Lahn rivers and it is part of the Rhenish Slate Mountains. On the opposite side of the Rhine, The Taunus range is continued by the Hunsrück. For geographical, ecological and geological purposes the Taunus is divided in three parts: *Anterior Taunus ''(Vortaunus'' or ''Vordertaunus)'' in the south ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diabase
Diabase (), also called dolerite () or microgabbro, is a mafic, holocrystalline, subvolcanic rock equivalent to volcanic basalt or plutonic gabbro. Diabase dikes and sills are typically shallow intrusive bodies and often exhibit fine-grained to aphanitic chilled margins which may contain tachylite (dark mafic glass). ''Diabase'' is the preferred name in North America, while ''dolerite'' is the preferred name in the rest of the English-speaking world, where sometimes the name ''diabase'' refers to altered dolerites and basalts. Some geologists prefer to avoid confusion by using the name ''microgabbro''. The name ''diabase'' comes from the French ', and ultimately from the Greek - meaning "act of crossing over, transition". Petrography Diabase normally has a fine but visible texture of euhedral lath-shaped plagioclase crystals (62%) set in a finer matrix of clinopyroxene, typically augite (20–29%), with minor olivine (3% up to 12% in olivine diabase), magnetite (2%), an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Hintertaunus
The Hintertaunus ("Farther Taunus") is a natural region in the German Central Upland range of the Taunus (major unit group 30), which rises to a height of and lies north of the High Taunus (301). It extends as far as the river Rhine to the west, the river Lahn to the north and the Wetterau hills to the east. It is divided into the Eastern Hintertaunus (major unit 302), Idstein Basin The Hintertaunus ("Farther Taunus") is a natural region in the German Central Upland range of the Taunus (major unit group 30), which rises to a height of and lies north of the High Taunus (301). It extends as far as the river Rhine to the w ... (303) and Western Hintertaunus (304). External links * Taunus {{Hesse-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mineral Spring
Mineral springs are naturally occurring springs that produces hard water, water that contains dissolved minerals. Salts, sulfur compounds, and gases are among the substances that can be dissolved in the spring water during its passage underground. In this they are unlike sweet springs, which produce soft water with no noticeable dissolved gasses. The dissolved minerals may alter the water's taste. Mineral water obtained from mineral springs, and the precipitated salts such as Epsom salt have long been important commercial products. Some mineral springs may contain significant amounts of harmful dissolved minerals, such as arsenic, and should not be drunk. Sulfur springs smell of rotten eggs due to hydrogen sulfide (H2S), which is hazardous and sometimes deadly. It is a gas, and it usually enters the body when it is breathed in. The quantities ingested in drinking water are much lower and are not considered likely to cause harm, but few studies on long-term, low-level exposu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dietkirchen (Limburg)
Dietkirchen an der Lahn is a borough (''Ortsbezirk'') of Limburg an der Lahn, seat of the district of Limburg-Weilburg in the state of Hesse, Germany. The formerly independent village was incorporated into Limburg in 1971. The town is dominated by the basilica St. Lubentius, which was the most important early-medieval church building in the region. Geography Dietkirchen is situated directly on the west (left) bank of the Lahn River. Its prominent feature is the towering limestone bluff on which St. Lubentius is built. The central town of Limburg is located in a widening of the Lahn valley. Dietkirchen is situated at the eastern end of this widening, with the valley becoming narrow again near Runkel. The old village is characterized by a large height differential, with housing plots situated on terraces formed by numerous retaining walls. The village itself is situated at an elevation of 120 to 170 meters. In the northern part of the borough, the landscape rises up to 180 mete ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Obertiefenbach (Beselich)
Obertiefenbach is a municipality in the district of Rhein-Lahn, in Rhineland-Palatinate, in western 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 .... References Rhein-Lahn-Kreis {{RheinLahn-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beselich
Beselich is a municipality in Limburg-Weilburg district in Hesse, Germany. Geography Location Beselich lies on the northeast edge of the Limburg Basin on the edge of the Lahn valley, on the southeast slope of the Westerwald 220 m above sea level. Visible from far away is the Beselicher Kopf (296 m). The brooks Tiefenbach, Kerkerbach and Brandbach flow through the municipal area. Twenty-two percent of Beselich's area is wooded. Geology The countryside is partly wooded and underlain with marble, clay, basalt and iron ore deposits. To this day, clay is still quarried in Obertiefenbach. The black marble from the Schupbach area is used worldwide. Among other instances, it was used in the Empire State Building in New York. Neighbouring communities The community of Beselich borders in the north on the communities of Merenberg and Waldbrunn, in the east on the town of Weilburg, in the south on the town of Runkel and the district seat of Limburg, also a town, and in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hadamar
Hadamar is a small town in Limburg-Weilburg district in Hesse, Germany. Hadamar is known for its Clinic for Forensic Psychiatry/Centre for Social Psychiatry, lying at the edge of town, in whose outlying buildings is also found the Hadamar Memorial. This remembers the murders of people with handicaps and mental illnesses under the Nazi regime at the ''NS-Tötungsanstalt Hadamar''.http://www.graf-von-katzenelnbogen.de/ The History of the County of Katzenelnbogen and the First Riesling of the World Geography Location Hadamar lies 7 km north of Limburg between Cologne and Frankfurt am Main on the southern edge of the Westerwald at elevations from 120 to 390 m above sea level. Neighbouring communities Hadamar borders in the north on the communities of Dornburg, Elbtal and Waldbrunn, in the east on the community of Beselich, in the south on the town of Limburg and the community of Elz (all in Limburg-Weilburg) and in the west on the community of Hundsangen (in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Galgenberg (Limburg Basin) , a prehistoric figurine discovered in 1988 near Stratzing, Austria
*
{{disambig, geo ...
Galgenberg is a German name corresponding to the English "Gallows Hill". Galgenberg may refer to: * Galgenberg (Elbingerode), a hill near Elbingerode in the Harz Mountains of central Germany * Galgenberg (Heilbronn), a mountain of Baden-Württemberg, Germany * Galgenberg (Lütte), a hill in Bad Belzig, Brandenburg, Germany * Galgenberg (Schwarzenberg), a mountain of Saxony, southeastern Germany * Galgenberg Formation, a fossiliferous geologic formation in Germany * Ouvrage Galgenberg, a portion of the Fortified Sector of Thionville of the Maginot Line See also * Gallows Hill (other) * Venus of Galgenberg __NOTOC__ The Venus of Galgenberg is a Venus figurine of the Aurignacian era, dated to about 30,000 years ago. The sculpture, also known in German as the Fanny von Galgenberg, was discovered in 1988 close to Stratzing, Austria, not far from the s ... [...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] |
.jpg "Click for more on -> Mineral Spring")
