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Karmelenberg Aufschluss
The Karmelenberg is a wooded cinder cone that was formed by volcanic activity. It marks the southeastern end of the East Eifel volcano field and rises to a height of , about 170 metres above the Pellenz region, and is visible from a long way off. In the UNO Year of Mountains (2002), the Karmelenberg was Mountain/Hill of the Month in Germany. A monument records the proclamation on 21 June 2002. As part of the Volcano Park (station 21), the hill is counted as a tourist attraction. Various information boards explain both its volcanic past as well as the history of St. Mary’s Chapel at the summit. The hill is named after Mount Carmel in the Carmel massif, an important Biblical site and modern landmark in northwestern Israel. The entire cinder cone of the Karmelenberg has been designated as a nature reserve. Location The Karmelenberg belongs to the municipality of Bassenheim and is situated close to the Ochtendung junction on the A 48 motorway. Nearby is the Goloring, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mayen-Koblenz
Mayen-Koblenz is a district (''Kreis'') in the north of Rhineland-Palatinate, Germany. Neighboring districts are (from north clockwise) Ahrweiler (district), Ahrweiler, Neuwied (district), Neuwied, Westerwaldkreis, district-free Koblenz, Rhein-Lahn, Rhein-Hunsrück, Cochem-Zell, and Vulkaneifel. History The district was created in 1973 when the two districts, Mayen and Koblenz, were merged. The district has been 'twinned' with the Borough of Waverley, Surrey, Waverley in Surrey in southern England since 1982. Geography The two main rivers of the district are the Rhine and the Moselle (river), Moselle, which join at the ''Deutsches Eck'' in Koblenz. In the west of the district are the Eifel mountains. These also include the large lake, the ''Laacher See'', a volcanic caldera formed 12000 years ago. Coat of arms The coat of arms combine the elements of the two precursor districts. The tree, a ''Maie'', is taken from the Mayen district. The wavy line represents the two rivers Rhine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Goloring
The Goloring is an ancient earthworks monument located near Koblenz, Germany. It was created in the Bronze Age era, which dates back to the Urnfield culture (1200–800 BCE.). During this time a widespread solar cult is believed to have existed in Central Europe. The Goloring consists of a circular ditch of 175 metres in diameter with an outside embankment extending to 190 metres. Technically this makes the structure a henge monument, although the use of the term henge outside of Britain is sometimes disputed. The outside embankment is approx. 7 metres wide and 80 cm high. The ditch has an upper width of 5–6 metres and is approx. 80 cm deep. In the interior one can find a roughly circular leveled platform, which is about elevated by about 1 metre. The platform has been created based on piled gravelled rock and has a diameter of 95 metres. Remnants of a 50 cm thick wooden post with an estimated height of 8–12 metres were excavated in the middle of this platform. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Volcanoes In Germany ...
This is a list of active and extinct volcanoes. See also *Volcanic Eifel References {{Global Volcanism Program Germany * Volcanoes Volcanoes A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Regierungsbezirk Koblenz
Koblenz was one of the - at last - three ''Regierungsbezirke'' of Rhineland-Palatinate, Germany, located in the north-east of the state. The region was created in 1815 as part of the Prussian Rhineland, becoming part of the new state of Rhineland-Palatinate in 1946. In 1968 the neighbouring Montabaur Region was dissolved and its territory annexed to Koblenz Region. Since 2000, the employees and assets of the Bezirksregierungen form the ''Aufsichts- und Dienstleistungsdirektion Trier'' (Supervisory and Service Directorate Trier) and the ''Struktur- und Genehmigungsdirektionen'' (Structural and Approval Directorates) ''Nord'' in Koblenz and ''Süd'' in Neustadt (Weinstraße). These administrations execute their authority over the whole state, i. e. the ''ADD Trier'' oversees all schools. ''Kreise''(districts) # Ahrweiler # Altenkirchen # Bad Kreuznach # Birkenfeld # Cochem-Zell # Mayen-Koblenz # Neuwied # Rhein-Hunsrück # Rhein-Lahn # Westerwaldkreis The Westerwaldkreis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hectare
The hectare (; SI symbol: ha) is a non-SI metric unit of area equal to a square with 100-metre sides (1 hm2), or 10,000 m2, and is primarily used in the measurement of land. There are 100 hectares in one square kilometre. An acre is about and one hectare contains about . In 1795, when the metric system was introduced, the ''are'' was defined as 100 square metres, or one square decametre, and the hectare ("hecto-" + "are") was thus 100 ''ares'' or km2 (10,000 square metres). When the metric system was further rationalised in 1960, resulting in the International System of Units (), the ''are'' was not included as a recognised unit. The hectare, however, remains as a non-SI unit accepted for use with the SI and whose use is "expected to continue indefinitely". Though the dekare/decare daa (1,000 m2) and are (100 m2) are not officially "accepted for use", they are still used in some contexts. Description The hectare (), although not a unit of SI, i ... [...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] |
Pumice
Pumice (), called pumicite in its powdered or dust form, is a volcanic rock that consists of highly vesicular rough-textured volcanic glass, which may or may not contain crystals. It is typically light-colored. Scoria is another vesicular volcanic rock that differs from pumice in having larger vesicles, thicker vesicle walls, and being dark colored and denser.Jackson, J.A., J. Mehl, and K. Neuendorf (2005) ''Glossary of Geology'' American Geological Institute, Alexandria, Virginia. 800 pp. McPhie, J., M. Doyle, and R. Allen (1993) ''Volcanic Textures A guide to the interpretation of textures in volcanic rocks'' Centre for Ore Deposit and Exploration Studies, University of Tasmania, Hobart, Tasmania..198 pp. Pumice is created when super-heated, highly pressurized rock is violently ejected from a volcano. The unusual foamy configuration of pumice happens because of simultaneous rapid cooling and rapid depressurization. The depressurization creates bubbles by lowering the solubi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lava
Lava is molten or partially molten rock (magma) that has been expelled from the interior of a terrestrial planet (such as Earth) or a moon onto its surface. Lava may be erupted at a volcano or through a fracture in the crust, on land or underwater, usually at temperatures from . The volcanic rock resulting from subsequent cooling is also often called ''lava''. A lava flow is an outpouring of lava during an effusive eruption. (An explosive eruption, by contrast, produces a mixture of volcanic ash and other fragments called tephra, not lava flows.) The viscosity of most lava is about that of ketchup, roughly 10,000 to 100,000 times that of water. Even so, lava can flow great distances before cooling causes it to solidify, because lava exposed to air quickly develops a solid crust that insulates the remaining liquid lava, helping to keep it hot and inviscid enough to continue flowing. The word ''lava'' comes from Italian and is probably derived from the Latin word ''labes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moselle
The Moselle ( , ; german: Mosel ; lb, Musel ) is a river that rises in the Vosges mountains and flows through north-eastern France and Luxembourg to western Germany. It is a bank (geography), left bank tributary of the Rhine, which it joins at Koblenz. A small part of Belgium is in its drainage basin, basin as it includes the Sauer and the Our River, Our. Its lower course "twists and turns its way between Trier and Koblenz along one of Germany's most beautiful river valleys."''Moselle: Holidays in one of Germany's most beautiful river valleys'' at www.romantic-germany.info. Retrieved 23 Jan 2016. In this section the land to the north is the Eifel which stretches into Belgium; to the south lies the Hunsrück. The river flows through a region that was cultivated by the Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hunsrück
The Hunsrück () is a long, triangular, pronounced upland in Rhineland-Palatinate, Germany. It is bounded by the valleys of the Moselle-Saar (north-to-west), the Nahe (south), and the Rhine (east). It is continued by the Taunus mountains, past the Rhine and by the Eifel past the Moselle. To the south of the Nahe is a lower, hilly country forming the near bulk of the Palatinate region and all of the, smaller, Saarland. Below its north-east corner is Koblenz. As the Hunsrück proceeds east it acquires north-south width and three notable gaps in its southern ridges. In this zone are multi-branch headwaters including the Simmerbach ending at Simmertal on the southern edge. This interior is therefore rarely higher than above sea level. Peaks and escarpments are principally: the (Black Forest) Hochwald, the Idar Forest, the Soonwald, and the Bingen Forest. The highest mountain is the Erbeskopf (816 m; 2,677 ft), towards the region's south-west. Notable towns are Simmern, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neuwied Basin
Neuwied () is a town in the north of the German state of Rhineland-Palatinate, capital of the Neuwied (district), District of Neuwied. Neuwied lies on the east bank of the Rhine, 12 km northwest of Koblenz, on the railway from Frankfurt am Main to Cologne. The town has 13 suburban administrative districts: Heimbach-Weis, Gladbach, Engers, Oberbieber, Niederbieber, Torney, Segendorf, Altwied, Block, Irlich, Feldkirchen, Heddesdorf and Rodenbach. The largest is Heimbach-Weis, with approximately 8000 inhabitants. History Near Neuwied, one of the largest Roman ''castra'' on the Rhine has been excavated by archeologists. Caesar's Rhine bridges are believed to have been built nearby. Neuwied was founded in 1653 by Count Frederick III. of County of Wied, Wied, initially as a fortress on the site of the village of Langendorf, which had been destroyed in the Thirty Years' War (1618–1648). It was to serve as the new residence of the lower county, secure its only access to the Rhi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
