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Büscheich-Niedereich
Gerolstein () is a town in the Vulkaneifel district of Rhineland-Palatinate, Germany. Gerolstein is a local municipality of the ''Verbandsgemeinde Gerolstein''. It has been approved as a ''Luftkurort'' (spa town). History As early as the Stone Age, there is evidence of human habitation in the ''Buchenloch'', a nearby cave. In the Bronze Age the Dietzenley was used by the Celts as a refuge castle. In Roman times a temple and dwellings were known to have existed, and remnants of them have been preserved. One form of the name Gerolstein first appeared in connection with the building of the Löwenburg in 1115, which was then named the ''Burg Gerhardstein''. Town rights were granted to Gerolstein in 1336. In 1691, the town was almost completely destroyed when it was liberated from French occupation by troops from the Duchy of Jülich. After reconstruction, a devastating fire burnt down the town in 1708, and again in 1784. In the 1801 Treaty of Lunéville, Gerolstein, along with a ...
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Dietzenley
The Dietzenley in the county of Vulkaneifel in the German state of Rhineland-Palatinate is a mountain, ,{{GeoQuelle, DE-RP, LANDIS-Karte and the highest point in the Pelm Forest, a part of the Volcanic Eifel range. The Dietzenley rises within the Volcanic Eifel Nature Park in the parish of Gerolstein north and above the Gerolstein quarter of Büscheich-Niedereich. On the largely wooded '' domed summit'' stands a small, wooden observation tower An observation tower is a structure used to view events from a long distance and to create a full 360 degree range of vision to conduct long distance observations. Observation towers are usually at least tall and are made from stone, iron, and ..., which offers a good view of the Volcanic Eifel. Somewhat below it there is an electrical converter and the remains of a Celtic ringwall. The Dietzenley may be reached on footpaths from Gerolstein, Pelm or Gees. References Mountains under 1000 metres Mountains and hills of the Eif ...
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Lissingen Castle
Lissingen Castle (german: Burg Lissingen) is a well-preserved former moated castle dating to the 13th century. It is located on the River Kyll in Gerolstein in the administrative district of Vulkaneifel in Rhineland-Palatinate, Germany. From the outside it appears to be a single unit, but it is a double castle; an estate division in 1559 created the so-called lower castle and upper castle, which continue to have separate owners. Together with Bürresheim Castle, Bürresheim and Eltz Castle, Eltz, it has the distinction among castles in the Eifel of never having been destroyed. Lissingen Castle is a protected cultural property under the Hague Convention for the Protection of Cultural Property in the Event of Armed Conflict, Hague Convention. Location The castle is located on the edge of Lissingen, a district of the city of Gerolstein, close to the river Kyll. It was originally surrounded by the river and on the south and west sides by a moat. The moat has been filled in and stre ...
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Rhine
The Rhine ; french: Rhin ; nl, Rijn ; wa, Rén ; li, Rien; rm, label=Sursilvan, Rein, rm, label=Sutsilvan and Surmiran, Ragn, rm, label=Rumantsch Grischun, Vallader and Puter, Rain; it, Reno ; gsw, Rhi(n), including in Alsatian dialect, Alsatian and Low Alemannic German; ksh, label=Ripuarian language, Ripuarian and Low Franconian languages, Low Franconian, Rhing; la, Rhenus ; hu, Rajna . is one of the major List of rivers of Europe, European rivers. The river begins in the Swiss canton of Graubünden in the southeastern Swiss Alps. It forms part of the Swiss-Liechtenstein, Swiss-Austrian border, Swiss-Austrian, Swiss-German border, Swiss-German borders. After that the Rhine defines much of the Franco-German border, after which it flows in a mostly northerly direction through the German Rhineland. Finally in Germany the Rhine turns into a predominantly westerly direction and flows into the Netherlands where it eventually empties into the North Sea. It drains an area of 9,9 ...
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Central Place Theory
Central place theory is an urban geographical theory that seeks to explain the number, size and range of market services in a commercial system or human settlements in a residential system.Goodall, B. (1987) The Penguin Dictionary of Human Geography. London: Penguin. It was introduced in 1933 to explain the spatial distribution of cities across the landscape. The theory was first analyzed by German geographer Walter Christaller, who asserted that settlements simply functioned as 'central places' providing economic services to surrounding areas. Christaller explained that a large number of small settlements will be situated relatively close to one another for efficiency, and because people don’t want to travel far for everyday needs, like getting bread from a bakery. But people would travel further for more expensive and infrequent purchases or specialized goods and services which would be located in larger settlements that are farther apart. Building the theory To develop the ...
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Basalt
Basalt (; ) is an 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 surface of a rocky planet or 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 Venus, which cover ~80% of the surface, are basaltic; the 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 flows that can spread over great areas before cooling and solidifying. Flood basalts are thick sequence ...
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Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite whic ...
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Kyll
The Kyll (), noted by the Roman poet Ausonius as ''Celbis'',Ausonius, ''Mosella'', v. 359 is a river in western Germany (North Rhine-Westphalia and Rhineland-Palatinate), left tributary of the Moselle. It rises in the Eifel mountains, near the border with Belgium and flows generally south through the towns Stadtkyll, Gerolstein, Kyllburg and east of Bitburg. It flows into the Moselle in Ehrang, a suburb of Trier. See also *List of rivers of North Rhine-Westphalia A list of rivers of North Rhine-Westphalia, Germany: A * Aa, left tributary of the Möhne * Aa, left tributary of the Nethe * Aa, left tributary of the Werre * Aabach, tributary of the Afte * Aabach, small river in the Ems river system *Abbabach ... * List of rivers of Rhineland-Palatinate References Rivers of North Rhine-Westphalia Rivers of Rhineland-Palatinate Rivers of the Eifel Rivers of Germany {{RhinelandPalatinate-river-stub ...
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Allies Of World War II
The Allies, formally referred to as the United Nations from 1942, were an international military coalition formed during the Second World War (1939–1945) to oppose the Axis powers, led by Nazi Germany, Imperial Japan, and Fascist Italy. Its principal members by 1941 were the United Kingdom, United States, Soviet Union, and China. Membership in the Allies varied during the course of the war. When the conflict broke out on 1 September 1939, the Allied coalition consisted of the United Kingdom, France, and Poland, as well as their respective dependencies, such as British India. They were soon joined by the independent dominions of the British Commonwealth: Canada, Australia, New Zealand and South Africa. Consequently, the initial alliance resembled that of the First World War. As Axis forces began invading northern Europe and the Balkans, the Allies added the Netherlands, Belgium, Norway, Greece, and Yugoslavia. The Soviet Union, which initially ha ...
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Railway
Rail transport (also known as train transport) is a means of transport that transfers passengers and goods on wheeled vehicles running on rails, which are incorporated in Track (rail transport), tracks. In contrast to road transport, where the vehicles run on a prepared flat surface, rail vehicles (rolling stock) are directionally guided by the tracks on which they run. Tracks usually consist of steel rails, installed on Railroad tie, sleepers (ties) set in track ballast, ballast, on which the rolling stock, usually fitted with metal wheels, moves. Other variations are also possible, such as "slab track", in which the rails are fastened to a concrete foundation resting on a prepared subsurface. Rolling stock in a rail transport system generally encounters lower friction, frictional resistance than rubber-tyred road vehicles, so passenger and freight cars (carriages and wagons) can be coupled into longer trains. The rail transport operations, operation is carried out by a ...
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Second World War
World War II or the Second World War, often abbreviated as WWII or WW2, was a world war that lasted from 1939 to 1945. It involved the World War II by country, vast majority of the world's countries—including all of the great powers—forming two opposing military alliances: the Allies of World War II, Allies and the Axis powers. World War II was a total war that directly involved more than 100 million Military personnel, personnel from more than 30 countries. The major participants in the war threw their entire economic, industrial, and scientific capabilities behind the war effort, blurring the distinction between civilian and military resources. Air warfare of World War II, Aircraft played a major role in the conflict, enabling the strategic bombing of population centres and deploying the Atomic bombings of Hiroshima and Nagasaki, only two nuclear weapons ever used in war. World War II was by far the List of wars by death toll, deadliest conflict in hu ...
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Mineral Water
Mineral water is water from a mineral spring that contains various minerals, such as salts and sulfur compounds. Mineral water may usually be still or sparkling (carbonated/effervescent) according to the presence or absence of added gases. Traditionally, mineral waters were used or consumed at their spring sources, often referred to as "taking the waters" or "taking the cure", at places such as spas, baths, or wells. The term ''spa'' was used for a place where the water was consumed and bathed in; ''bath'' where the water was used primarily for bathing, therapeutics, or recreation; and ''well'' where the water was to be consumed. Today, it is far more common for mineral water to be bottled at the source for distributed consumption. Travelling to the mineral water site for direct access to the water is now uncommon, and in many cases not possible because of exclusive commercial ownership rights. There are more than 4,000 brands of mineral water commercially available worldwide ...
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Spring (hydrology)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels thr ...
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