RHINO Germany - Home of Music. Gefällt Mal · Personen sprechen darüber. #Roots #Sounds #Memories Spannende Hintergrundinfos aus der. Vorstellungen Alben, Vinyl und Box-Sets. Erinnerungen an Songs, Konzerte und Trends aus allen boulecentrum.nu das ist RHINO Germany - Home Of Music! Rhina is a village in eastern Hesse, Germany, belonging to the Haunetal municipality within the district of Hersfeld-Rotenburg. In , the population of Rhina.
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Rhina is a village in eastern Hesse, Germany, belonging to the Haunetal municipality within the district of Hersfeld-Rotenburg. In , the population of Rhina. ↑ Denkmaltopographie Bundesrepublik Deutschland, Reihe "Kulturdenkmäler in Hessen", Band 18, Landkreis Hersfeld-Rotenburg I, hg. von Ellen Kemp. Geni Project: Jewish Families from Rhina (Hessen), Germany. This project seeks to collect all of the Jewish families from the town of Rhina. Spannende Stories aus mehr als 50 Jahren Musikgeschichte gibt's bei Rhino Germany - Home of Music. RHINO Germany - Home of Music. likes · talking about this. #Roots #Sounds #Memories Spannende Hintergrundinfos aus der Popkultur und zu. RHINO Germany - Home of Music. Gefällt Mal · Personen sprechen darüber. #Roots #Sounds #Memories Spannende Hintergrundinfos aus der. Das aktuelle Wetter in Rhina (Hessen, Deutschland) mit ausführlichen Informationen zur Wetterlage.
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GPX File. LOC File. The quarter has about inhabitants and is the district with the most industrial jobs. In the 1st to 3rd century, there was a large Roman agricultural estate here.
Under the name Rhina it was first mentioned in It then belonged to the abbey of Säckingen and was part of the parish Murg.
In Rhina was separated from Murg and became an independent municipality. Between and , the world's first river hydropower plant, which stands across the river, was built in the Rhine.
It was the most powerful hydropower plant in Europe at the start of operation and became the classic model for today's run-of-river power plants.
After only years of independence, Rhina was re-incorporated in , not back to Murg, but by Laufenburg in the east. The town hall: The former Rhina town hall is a two-story house with a large copper-clad ridge turret with clocks, and a far projecting staircase section on the west side.
Above the entrance there is a mural of a fir on a river, the former coat of arms of the municipality. The house was built around as town hall and school of the new municipality.
In it lost its function and was sold to private owners. The renovation of the house in was awarded a prize. Das Quartier hat rund Einwohner und ist der Stadtteil mit den meisten industriellen Arbeitsplätzen.
Jahrhundert befand sich hier ein grosser römischer Gutshof. During the Reformation, the local production of pottery developed in the village.
The first evidence of the presence of Jews in the village is documented from during the Thirty Years War.
From the 18th century especially, the Jewish community grew at a regular rate, the first synagogue being erected in In , Rhina came under the rule of the Kingdom of Westphalia.
The church of Rhina was re-built in In , Rhina was incorporated into the Hünfeld district of the Hessian province of Fulda. Rhina's synagogue was rebuilt from to In , the first village-wide local elections were held.
A Jewish cemetery was created in The residents of the villages of Wehrda, Rhina, Schletzenrod, and Wetzlos rebelled against the noble lordship of the region in the Revolution of In the course of the conflict, attacks were also carried out against Rhina's Jews.
In , following a great increase in the Jewish population of Rhinda, a Jewish grade school was opened. Rhina received its first telephone in , and in developed water and plumbing infrastructure.
In , following an order by the NSDAP district leadership as well as the office of the regional administration, the Jewish members of the municipal council were forced to resign from their posts.
From , assaults on Jewish property and against those of Jewish faith began to occur. In , those attending the synagogue were beaten up.The church of Rhina was originally consecrated in the name of St. Here the ones we know: Rhina. Lost Room Staffel 2 3,8 mi Hermann-Lietz-Str. Published: December 15, Length: min Rating: 5 of 5 Author: ackerbauerroos. Wikipedia Article Mountains of Hesse. Views Read Edit View history. Der Hengst ist fair nach den Im Last Update: Travel warnings are updated daily. Safety Score: 3,5 of 5. Ina village community center was dedicated on the Sloth German site American Ganstar Rhina's synagogue. Wikipedia Article Municipalities in Hesse. Lotto Registrieren Ort wurde erstmals urkundlich erwähnt. Am westlichen Rand des Dorfes liegt am kleinen Rhina-Bach die Rhinmühle, die bereits in Jeck Pot schriftlichen Überlieferung auftauchte. Inthose attending the synagogue were beaten up. Hey, mein erstes Video was ich mit Live Blackjack T-Rex aufgenommen habe. Rhina was greatly affected by floods after an overflowing of the Haune River in
The gorge is quite deep and is the stretch of the river which is known for its many castles and vineyards. Between Strasbourg and Kehl. Aerial photo between Eltville and Bingen.
Marksburg near Koblenz , built in Ludendorff Bridge at Remagen , showing damage before collapse during the Battle of Remagen.
In this sections the river falls from On the left, is located the mountain ranges of Hunsrück and Eifel , on the right Taunus and Westerwald. According to geologists, the characteristic narrow valley form was created by erosion by the river while the surrounding landscape was lifted see water gap.
Major tributaries in this section are the Lahn and the Moselle. They join the Rhine near Koblenz , for the right and left respectively.
The dominant economic sectors in the Middle Rhine area are viniculture and tourism. Near Sankt Goarshausen , the Rhine flows around the famous rock Lorelei.
With its outstanding architectural monuments, the slopes full of vines, settlements crowded on the narrow river banks and scores of castles lined up along the top of the steep slopes, the Middle Rhine Valley can be considered the epitome of the Rhine romanticism.
The main tributaries on this stretch are the Ruhr and the Lippe. Like the Upper Rhine, the Lower Rhine used to meander until engineering created a solid river bed.
Because the levees are some distance from the river, at high tide the Lower Rhine has more room for widening than the Upper Rhine. Its banks are usually heavily populated and industrialized, in particular the agglomerations Cologne , Düsseldorf and Ruhr area.
Here the Rhine flows through the largest conurbation in Germany, the Rhine-Ruhr region. One of the most important cities in this region is Duisburg with the largest river port in Europe Duisport.
The region downstream of Duisburg is more agricultural. Near Krefeld , the river crosses the Uerdingen line , the line which separates the areas where Low German and High German are spoken.
Until the early s, industry was a major source of water pollution. Although many plants and factories can be found along the Rhine up into Switzerland , it is along the Lower Rhine that the bulk of them are concentrated, as the river passes the major cities of Cologne , Düsseldorf and Duisburg.
Duisburg is the home of Europe's largest inland port and functions as a hub to the sea ports of Rotterdam , Antwerp and Amsterdam.
The Ruhr , which joins the Rhine in Duisburg, is nowadays a clean river, thanks to a combination of stricter environmental controls, a transition from heavy industry to light industry and cleanup measures, such as the reforestation of Slag and brownfields.
The Ruhr currently provides the region with drinking water. Other rivers in the Ruhr Area , above all, the Emscher , still carry a considerable degree of pollution.
The Dutch name for Rhine is "Rijn". From here, the situation becomes more complicated, as the Dutch name Rijn no longer coincides with the main flow of water.
Two-thirds of the water flow volume of the Rhine flows farther west, through the Waal and then, via the Merwede and Nieuwe Merwede De Biesbosch , merging with the Meuse, through the Hollands Diep and Haringvliet estuaries , into the North Sea.
The other third of the water flows through the Pannerdens Kanaal and redistributes in the IJssel and Nederrijn.
The IJssel branch carries one ninth of the water flow of the Rhine north into the IJsselmeer a former bay , while the Nederrijn carries approximately two-ninths of the flow west along a route parallel to the Waal.
However, at Wijk bij Duurstede , the Nederrijn changes its name and becomes the Lek. The name Rijn , from here on, is used only for smaller streams farther to the north, which together formed the main river Rhine in Roman times.
Though they retained the name, these streams no longer carry water from the Rhine, but are used for draining the surrounding land and polders.
The latter flows west into a sluice at Katwijk , where its waters can be discharged into the North Sea. This branch once formed the line along which the Limes Germanicus were built.
During periods of lower sea levels within the various ice ages, the Rhine took a left turn, creating the Channel River , the course of which now lies below the English Channel.
Since the Rhine contributes most of the water, the shorter term Rhine Delta is commonly used. However, this name is also used for the river delta where the Rhine flows into Lake Constance , so it is clearer to call the larger one Rhine-Meuse delta , or even Rhine—Meuse—Scheldt delta , as the Scheldt ends in the same delta.
The shape of the Rhine delta is determined by two bifurcations : first, at Millingen aan de Rijn , the Rhine splits into Waal and Pannerdens Kanaal , which changes its name to Nederrijn at Angeren , and second near Arnhem , the IJssel branches off from the Nederrijn.
This creates three main flows, two of which change names rather often. The middle flow begins as Nederrijn , then changes into Lek , then joins the Noord, thereby forming Nieuwe Maas.
Three more flows carry significant amounts of water: the Nieuwe Merwede "New Merwede" , which branches off from the southern branch where it changes from Boven to Beneden Merwede; the Oude Maas "Old Meuse" , which branches off from the southern branch where it changes from Beneden Merwede into Noord, and Dordtse Kil , which branches off from Oude Maas.
Before the St. Elizabeth's flood , the Meuse flowed just south of today's line Merwede-Oude Maas to the North Sea and formed an archipelago -like estuary with Waal and Lek.
This system of numerous bays, estuary-like extended rivers, many islands and constant changes of the coastline, is hard to imagine today. From to , the Meuse and Waal merged further upstream at Gorinchem to form Merwede.
For flood protection reasons, the Meuse was separated from the Waal through a lock and diverted into a new outlet called " Bergse Maas ", then Amer and then flows into the former bay Hollands Diep.
The northwestern part of the estuary around Hook of Holland , is still called Maasmond "Meuse Mouth" , ignoring the fact that it now carries only water from the Rhine.
This might explain the confusing naming of the various branches. The hydrography of the current delta is characterized by the delta's main arms, disconnected arms Hollandse IJssel , Linge , Vecht , etc.
Many rivers have been closed "dammed" and now serve as drainage channels for the numerous polders. The construction of Delta Works changed the Delta in the second half of the 20th Century fundamentally.
The Rhine-Meuse Delta is a tidal delta, shaped not only by the sedimentation of the rivers, but also by tidal currents.
This meant that high tide formed a serious risk because strong tidal currents could tear huge areas of land into the sea.
Before the construction of the Delta Works, tidal influence was palpable up to Nijmegen, and even today, after the regulatory action of the Delta Works, the tide acts far inland.
At the Waal, for example, the most landward tidal influence can be detected between Brakel and Zaltbommel. The Rhine flows from the Alps to the North Sea Basin ; the geography and geology of its present-day watershed has been developing, since the Alpine orogeny began.
The present Mediterranean Sea descends from this somewhat larger Tethys sea. Several microplates were caught in the squeeze and rotated or were pushed laterally, generating the individual features of Mediterranean geography: Iberia pushed up the Pyrenees ; Italy , the Alps, and Anatolia , moving west, the mountains of Greece and the islands.
The compression and orogeny continue today, as shown by the ongoing raising of the mountains a small amount each year and the active volcanoes.
In northern Europe, the North Sea Basin had formed during the Triassic and Jurassic periods and continued to be a sediment receiving basin since.
In between the zone of Alpine orogeny and North Sea Basin subsidence, remained highlands resulting from an earlier orogeny Variscan , such as the Ardennes , Eifel and Vosges.
From the Eocene onwards, the ongoing Alpine orogeny caused a N—S rift system to develop in this zone. The main elements of this rift are the Upper Rhine Graben , in southwest Germany and eastern France and the Lower Rhine Embayment, in northwest Germany and the southeastern Netherlands.
By the time of the Miocene, a river system had developed in the Upper Rhine Graben , that continued northward and is considered the first Rhine river.
At that time, it did not yet carry discharge from the Alps; instead, the watersheds of the Rhone and Danube drained the northern flanks of the Alps.
The watershed of the Rhine reaches into the Alps today, but it did not start out that way. The Rhine then had the Sieg as a tributary, but not yet the Moselle.
The northern Alps were then drained by the Danube. Through stream capture , the Rhine extended its watershed southward. By the Pliocene period, the Rhine had captured streams down to the Vosges Mountains , including the Main and the Neckar.
The northern Alps were then drained by the Rhone. Around 2. In the Early Pleistocene, the Rhine followed a course to the northwest, through the present North Sea.
This caused the Rhine's course to be diverted through the English Channel. Since then, during glacial times, the river mouth was located offshore of Brest, France and rivers, like the River Thames and the Seine , became tributaries to the Rhine.
During interglacials, when sea level rose to approximately the present level, the Rhine built deltas, in what is now the Netherlands.
The last phase slightly predates the global last ice age maximum Last Glacial Maximum. During this time, the lower Rhine flowed roughly west through the Netherlands and extended to the southwest, through the English Channel and finally, to the Atlantic Ocean.
Most of the Rhine's current course was not under the ice during the last Ice Age; although, its source must still have been a glacier.
Such was the case during the Last Glacial Maximum , ca. Loess wind-blown topsoil dust arose from the south and North Sea plain settling on the slopes of the Alps, Urals and the Rhine Valley, rendering the valleys facing the prevailing winds especially fertile.
As northwest Europe slowly began to warm up from 22, years ago onward, frozen subsoil and expanded alpine glaciers began to thaw and fall-winter snow covers melted in spring.
Much of the discharge was routed to the Rhine and its downstream extension. With globally shrinking ice-cover, ocean water levels rose and the English Channel and North Sea re-inundated.
Meltwater, adding to the ocean and land subsidence , drowned the former coasts of Europe transgressionally.
About years ago, the Rhine estuary was in the Strait of Dover. There remained some dry land in the southern North Sea , known as Doggerland , connecting mainland Europe to Britain.
Man was already resident in the area when these events happened. Since years ago the situation of tides, currents and land-forms has resembled the present.
Rates of sea level rise dropped such that natural sedimentation by the Rhine and coastal processes widely compensate for transgression by the sea.
About — BP, a general warming encouraged migration of all former ice-locked areas, including up the Danube and down the Rhine by peoples to the east.
As a meandering river, it reworked its ice-age floodplain. Coeval absolute sea-level rise and tectonic subsidence have strongly influenced delta evolution.
Other factors of importance to the shape of the delta are the local tectonic activities of the Peel Boundary Fault, the substrate and geomorphology, as inherited from the Last Glacial and the coastal-marine dynamics, such as barrier and tidal inlet formations.
As a result of increasing land clearance Bronze Age agriculture , in the upland areas central Germany , the sediment load of the Rhine has strongly increased  and delta growth has speeded up.
In the geologically recent past the main process distributing sediment across the delta has been the shifting of river channels to new locations on the floodplain termed avulsion.
This was followed by embankment of the major distributaries and damming of minor distributaries, which took place in the 11—13th century AD.
Thereafter, canals were dug, bends were straightened and groynes were built to prevent the river's channels from migrating or silting up.
The river IJssel branch flows to the north and enters the IJsselmeer formerly the Zuider Zee , initially a brackish lagoon but a freshwater lake since This discharge distribution has been maintained since by river engineering works including the digging of the Pannerdens canal and the installation, in the 20th century, of a series of weirs on the Nederrijn.
The Rhine was not known to Herodotus and first enters the historical period in the 1st century BC in Roman-era geography.
At that time, it formed the boundary between Gaul and Germania. In Roman geography, the Rhine formed the boundary between Gallia and Germania by definition; e.
In Roman geography, the Rhine and Hercynia Silva were considered the boundary of the civilized world; as it was a wilderness, the Romans were eager to explore it.
This view is typified by Res Gestae Divi Augusti , a long public inscription of Augustus , in which he boasts of his exploits; including, sending an expeditionary fleet north of the Rheinmouth, to Old Saxony and Jutland , which he claimed no Roman had ever done before.
At this time, the plain of the Lower Rhine was the territory of the Ubii. Beyond these rivers she held only the fertile plain of Frankfurt , opposite the Roman border fortress of Moguntiacum Mainz , the southernmost slopes of the Black Forest and a few scattered bridge-heads.
The northern section of this frontier, where the Rhine is deep and broad, remained the Roman boundary until the empire fell.
The southern part was different. The upper Rhine and upper Danube are easily crossed. The frontier which they form is inconveniently long, enclosing an acute-angled wedge of foreign territory between the modern Baden and Württemberg.
The Germanic populations of these lands seem in Roman times to have been scanty, and Roman subjects from the modern Alsace-Lorraine had drifted across the river eastwards.
The Romans kept eight legions in five bases along the Rhine. The number was reduced to four as more units were moved to the Danube.
The actual number of legions present at any base or in all, depended on whether a state or threat of war existed. The two original military districts of Germania Inferior and Germania Superior , came to influence the surrounding tribes, who later respected the distinction in their alliances and confederations.
For example, the upper Germanic peoples combined into the Alemanni. For a time, the Rhine ceased to be a border, when the Franks crossed the river and occupied Roman-dominated Celtic Gaul , as far as Paris.
This " Germanic Heroic Age " is reflected in medieval legend, such as the Nibelungenlied which tells of the hero Siegfried killing a dragon on the Drachenfels Siebengebirge "dragons rock" , near Bonn at the Rhine and of the Burgundians and their court at Worms, at the Rhine and Kriemhild's golden treasure, which was thrown into the Rhine by Hagen.
By the 6th century, the Rhine was within the borders of Francia. In the 9th, it formed part of the border between Middle and Western Francia , but in the 10th century, it was fully within the Holy Roman Empire , flowing through Swabia , Franconia and Lower Lorraine.
The mouths of the Rhine, in the county of Holland , fell to the Burgundian Netherlands in the 15th century; Holland remained contentious territory throughout the European wars of religion and the eventual collapse of the Holy Roman Empire, when the length of the Rhine fell to the First French Empire and its client states.
The numerous historic castles in Rhineland-Palatinate attest to the importance of the river as a commercial route. Establishing " natural borders " on the Rhine was a long-term goal of French foreign policy, since the Middle Ages , though the language border was — and is — far more to the west.
The Confederation of the Rhine was established by Napoleon, as a French client state , in and lasted until , during which time it served as a significant source of resources and military manpower for the First French Empire.
In , the Rhine crisis , prompted by French prime minister Adolphe Thiers 's desire to reinstate the Rhine as a natural border, led to a diplomatic crisis and a wave of nationalism in Germany.
The Rhine became an important symbol in German nationalism during the formation of the German state in the 19th century see Rhine romanticism.
This decreed that it would be occupied by the allies, until and after that, it would be a demilitarised zone, with the German army forbidden to enter.
The Treaty of Versailles and this particular provision, in general, caused much resentment in Germany and is often cited as helping Adolf Hitler 's rise to power.
The allies left the Rhineland, in and the German army re-occupied it in , which was enormously popular in Germany. Although the allies could probably have prevented the re-occupation, Britain and France were not inclined to do so, a feature of their policy of appeasement to Hitler.
In a separate operation, the Ludendorff Bridge , crossing the Rhine at Remagen , became famous, when U. This also became the subject of a film, The Bridge at Remagen.
Until the generally accepted length of the Rhine was 1, kilometres miles. In the German encyclopedia Knaurs Lexikon stated the length as 1, kilometres miles , presumably a typographical error.
After this number was placed into the authoritative Brockhaus Enzyklopädie, it became generally accepted and found its way into numerous textbooks and official publications.
The error was discovered in , and the Dutch Rijkswaterstaat confirms the length at 1, kilometres miles. During its course from the Alps to the North Sea, the Rhine passes through four countries and constitutes six different country borders.
On the various parts:. From Wikipedia, the free encyclopedia. This article is about the river. For other uses, see Rhine disambiguation and Rhein disambiguation.
River in Western Europe. The Rhine in Basel , Switzerland. Cologne Düsseldorf Rotterdam Strasbourg Basel. Main article: Sources of the Rhine. Main articles: Vorderrhein and Hinterrhein river.
Main article: Alpine Rhine. See also: Rheintal. Main article: Lake Constance. Main article: Obersee Lake Constance. Main article: Seerhein.
Main article: Untersee Lake Constance. Main article: High Rhine. Main article: Upper Rhine. Main article: Middle Rhine.
Play media. Rhine at Düsseldorf. Rhine at Hünxe , near the border of the Netherlands. Main article: Lower Rhine. Main article: Rhineland.
Further information: Rhenus Pater. This section does not cite any sources. Please help improve this section by adding citations to reliable sources.
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This list contains brief abstracts about monuments, holiday activities, national parcs, museums, organisations and more from the area as well as interesting facts about the region itself.
Where available, you'll find the corresponding homepage. Otherwise the related wikipedia article. The Aar, a tributary of the High Rhine, is the longest river that both rises and ends entirely within Switzerland.
Located at Waldshut is a district Kreis in the south of Baden-Württemberg, Germany. Neighbouring districts are clockwise from the west Lörrach, Breisgau-Hochschwarzwald and Schwarzwald-Baar; followed in the south by the Swiss cantons of Schaffhausen, Zürich and Aargau.
Brugg District is a district in the Canton of Aargau, Switzerland, it is located south of the Aare and the Aargauer Jura covers the district.
The capital of the district is the town of Brugg. Wikipedia Article Districts of Aargau. The Fricktal "Frick Valley" region is the northwest finger extending from the Swiss canton of Aargau.
It is situated in Northwestern Switzerland east of Basel, between the High Rhine forming the border with Germany in the north and the Jura Mountains in the south.
The Fricktal contains the districts of Laufenburg and Rheinfelden. The region is named after its former chief village Frick.
Wikipedia Article Regions of Switzerland. Except for the chapel, the green and orange colored buildings still exist today.
At the time of its construction, the location was part of the Duchy of Swabia. Stilli is a former municipality of the canton of Aargau, Switzerland.
On 1 January , it merged with its neighbouring municipality, Villigen. Laufenburg District is a district of the canton of Aargau, Switzerland, essentially consisting of the upper Fricktal valley in the Aargau Jura south of the Rhine.
Its capital is the town of Laufenburg. It has a population of 29, as of 30 June Benkerjoch Pass el. It connects Küttigen and Oberhof.
Until , the pass was the boundary between Austria and Switzerland. The current pass road was built in A postal bus route runs over the pass to Aarau.
Bözberg Pass el. Two tunnels have been dug under the pass, one for the Federal Railway and one for the A-3 Autobahn.
Salhöhe Pass el. It connects Kienberg in Solothurn and Erlinsbach in Aargau. The pass road has a maximum grade of 9 percent.
Although it is the shortest route between Aarau and Basel, traffic over the pass is moderate. Staffelegg Pass el. It connects Küttigen and Asp.
The postal bus route from Frick to Aarau goes over the pass, and there is a restaurant at the summit. The Möhlintal is a kilometre long valley running between Möhlin and Wegenstetten in the Rheinfelden district of Canton Aargau, Switzerland.
The five municipalities in the valley have a total population of around 14, people. In the upper valley, the valley is also known as the "Wegenstettertal".
This name was particularly used by associations and groups related to the upper Möhlintal municipalities. In Habsburg times the area Landschaft territory Möhlinbach was already known.
Wikipedia Article Geography of Aargau. It is located west of the village on a rocky outcrop, surrounded by vineyards and woods.
Today, it serves as a boarding school for students with behavioral problems. The immediately adjacent castle Ruchenstein was demolished in , when the small fort was rebuilt into a Schloss Kasteln.
Iberg Castle is a ruined castle located on Iberg mountain in the municipality of Riniken in the canton of Aargau in Switzerland.
Only a few remnants of the ruins are visible. Schenkenberg Castle is a castle ruin above the municipality of Thalheim in the canton of Aargau in Switzerland.
It was built in the 13th Century by the Habsburg dynasty, was the administrative seat for years of a bailiwick of the city of Bern and fell into ruin in the 18th century.Local time in Rhina Welche Aufgaben Hatte Der Pharao now AM Wednesday. Im Reformationszeitalter ist im Dorf auch Pokerstrars örtlich produzierende Töpferei nachweisbar. Nikolaus geweiht. This list contains brief abstracts about monuments, holiday activities, national parcs, museums, organisations and more from the area as well as interesting facts about the Sunmaker Oder Stargames itself. November wurden die Synagoge und die räumlich integrierte jüdische Schule niedergebrannt. Euroleague Stats Live synagogue was rebuilt from to