The Rhine is one of the major European rivers, which has its sources in Switzerland and flows in an northerly direction through Germany and The Netherlands to the North Sea. The river begins in the Swiss canton of Graubünden in the southeastern Swiss Alps, forms part of the Swiss-Liechtenstein, Swiss-Austrian, Swiss-German and the Franco-German border flows through the German Rhineland and the Netherlands and empties into the North Sea; the largest city on the Rhine is Cologne, with a population of more than 1,050,000 people. It is the second-longest river in Central and Western Europe, at about 1,230 km, with an average discharge of about 2,900 m3/s; the Rhine and the Danube formed most of the northern inland frontier of the Roman Empire and, since those days, the Rhine has been a vital and navigable waterway carrying trade and goods deep inland. Its importance as a waterway in the Holy Roman Empire is supported by the many castles and fortifications built along it. In the modern era, it has become a symbol of German nationalism.
Among the biggest and most important cities on the Rhine are Cologne, Düsseldorf, Rotterdam and Basel. The variants of the name of the Rhine in modern languages are all derived from the Gaulish name Rēnos, adapted in Roman-era geography as Greek Ῥῆνος, Latin Rhenus; the spelling with Rh- in English Rhine as well as in German Rhein and French Rhin is due to the influence of Greek orthography, while the vocalisation -i- is due to the Proto-Germanic adoption of the Gaulish name as *Rīnaz, via Old Frankish giving Old English Rín,Old High German Rīn, early Middle Dutch Rijn. The diphthong in modern German Rhein is a Central German development of the early modern period, the Alemannic name Rī retaining the older vocalism, as does Ripuarian Rhing, while Palatine has diphthongized Rhei, Rhoi. Spanish is with French in adopting the Germanic vocalism Rin-, while Italian and Portuguese retain the Latin Ren-; the Gaulish name Rēnos belongs to a class of river names built from the PIE root *rei- "to move, run" found in other names such as the Reno in Italy.
The grammatical gender of the Celtic name is masculine, the name remains masculine in German and French. The Old English river name was variously inflected as feminine; the length of the Rhine is conventionally measured in "Rhine-kilometers", a scale introduced in 1939 which runs from the Old Rhine Bridge at Constance to Hoek van Holland. The river is shortened from its natural course due to a number of canalisation projects completed in the 19th and 20th century; the "total length of the Rhine", to the inclusion of Lake Constance and the Alpine Rhine is more difficult to measure objectively. Its course is conventionally divided as follows: The Rhine carries its name without distinctive accessories only from the confluence of the Rein Anteriur/Vorderrhein and Rein Posteriur/Hinterrhein next to Reichenau in Tamins. Above this point is the extensive catchment of the headwaters of the Rhine, it belongs exclusively to the Swiss canton of Graubünden, ranging from Saint-Gotthard Massif in the west via one valley lying in Ticino and Italy in the south to the Flüela Pass in the east.
Traditionally, Lake Toma near the Oberalp Pass in the Gotthard region is seen as the source of the Anterior Rhine and the Rhine as a whole. The Posterior Rhine rises in the Rheinwald below the Rheinwaldhorn; the source of the river is considered north of Lai da Tuma/Tomasee on Rein Anteriur/Vorderrhein, although its southern tributary Rein da Medel is longer before its confluence with the Anterior Rhine near Disentis. The Anterior Rhine springs from Lai da Tuma/Tomasee, near the Oberalp Pass and passes the impressive Ruinaulta formed by the largest visible rock slide in the alps, the Flims Rockslide; the Posterior Rhine starts near the Rheinwaldhorn. One of its tributaries, the Reno di Lei, drains the Valle di Lei on politically Italian territory. After three main valleys separated by the two gorges and Viamala, it reaches Reichenau in Tamins; the Anterior Rhine arises from numerous source streams in the upper Surselva and flows in an easterly direction. One source is Lai da Tuma with the Rein da Tuma, indicated as source of the Rhine, flowing through it.
Into it flow tributaries from the south, some longer, some equal in length, such as the Rein da Medel, the Rein da Maighels, the Rein da Curnera. The Cadlimo Valley in the canton of Ticino is drained by the Reno di Medel, which crosses the geomorphologic Alpine main ridge from the south. All streams in the source area are sometimes captured and sent to storage reservoirs for the local hydro-electric power plants; the culminating point of the Anterior Rhine's drainage basin is the Piz Russein of the Tödi massif of the Glarus Alps at 3,613 metres above sea level. It starts with the creek Aua da Russein. In its lower course the Anterior Rhine flows through a gorge named Ruinaulta; the whole stretch of the Anterior Rhine to the Alpine Rhine confluence next to Reichen
The North Sea is a marginal sea of the Atlantic Ocean located between the United Kingdom, Norway, Germany, the Netherlands and France. An epeiric sea on the European continental shelf, it connects to the ocean through the English Channel in the south and the Norwegian Sea in the north, it is more than 970 kilometres long and 580 kilometres wide, with an area of 570,000 square kilometres. The North Sea has long been the site of important European shipping lanes as well as a major fishery; the sea is a popular destination for recreation and tourism in bordering countries and more has developed into a rich source of energy resources including fossil fuels and early efforts in wave power. The North Sea has featured prominently in geopolitical and military affairs in Northern Europe, it was important globally through the power northern Europeans projected worldwide during much of the Middle Ages and into the modern era. The North Sea was the centre of the Vikings' rise. Subsequently, the Hanseatic League, the Netherlands, the British each sought to dominate the North Sea and thus access to the world's markets and resources.
As Germany's only outlet to the ocean, the North Sea continued to be strategically important through both World Wars. The coast of the North Sea presents a diversity of geographical features. In the north, deep fjords and sheer cliffs mark the Norwegian and Scottish coastlines, whereas in the south, the coast consists of sandy beaches and wide mudflats. Due to the dense population, heavy industrialization, intense use of the sea and area surrounding it, there have been various environmental issues affecting the sea's ecosystems. Adverse environmental issues – including overfishing and agricultural runoff and dumping, among others – have led to a number of efforts to prevent degradation of the sea while still making use of its economic potential; the North Sea is bounded by the Orkney Islands and east coast of Great Britain to the west and the northern and central European mainland to the east and south, including Norway, Germany, the Netherlands and France. In the southwest, beyond the Straits of Dover, the North Sea becomes the English Channel connecting to the Atlantic Ocean.
In the east, it connects to the Baltic Sea via the Skagerrak and Kattegat, narrow straits that separate Denmark from Norway and Sweden respectively. In the north it is bordered by the Shetland Islands, connects with the Norwegian Sea, which lies in the north-eastern part of the Atlantic; the North Sea is more than 970 kilometres long and 580 kilometres wide, with an area of 570,000 square kilometres and a volume of 54,000 cubic kilometres. Around the edges of the North Sea are sizeable islands and archipelagos, including Shetland and the Frisian Islands; the North Sea receives freshwater from a number of European continental watersheds, as well as the British Isles. A large part of the European drainage basin empties into the North Sea, including water from the Baltic Sea; the largest and most important rivers flowing into the North Sea are the Elbe and the Rhine – Meuse watershed. Around 185 million people live in the catchment area of the rivers discharging into the North Sea encompassing some industrialized areas.
For the most part, the sea lies on the European continental shelf with a mean depth of 90 metres. The only exception is the Norwegian trench, which extends parallel to the Norwegian shoreline from Oslo to an area north of Bergen, it has a maximum depth of 725 metres. The Dogger Bank, a vast moraine, or accumulation of unconsolidated glacial debris, rises to a mere 15 to 30 m below the surface; this feature has produced the finest fishing location of the North Sea. The Long Forties and the Broad Fourteens are large areas with uniform depth in fathoms; these great banks and others make the North Sea hazardous to navigate, alleviated by the implementation of satellite navigation systems. The Devil's Hole lies 200 miles east of Scotland; the feature is a series of asymmetrical trenches between 20 and 30 kilometres long and two kilometres wide and up to 230 metres deep. Other areas which are less deep are Fisher Bank and Noordhinder Bank; the International Hydrographic Organization defines the limits of the North Sea as follows: On the Southwest.
A line joining the Walde Lighthouse and Leathercoat Point. On the Northwest. From Dunnet Head in Scotland to Tor Ness in the Island of Hoy, thence through this island to the Kame of Hoy on to Breck Ness on Mainland through this island to Costa Head and to Inga Ness in Westray through Westray, to Bow Head, across to Mull Head and on to Seal Skerry and thence to Horse Island. On the North. From the North point of the Mainland of the Shetland Islands, across to Graveland Ness in the Island of Yell, through Yell to Gloup Ness and across to Spoo Ness in Unst island, through Unst to Herma Ness, on to the SW point of the Rumblings and to Muckle Flugga all these being included in the North Sea area.
Canal de Huningue
The Canal de Huningue is a canal in eastern France connecting the Rhine at Huningue to Niffer. The locks are no longer operational; the canal was enlarged in 1961 between Grand Canal Mulhouse. At the same time, the canal between Mulhouse and Friesenheim was closed to traffic as it had been duplicated by the Grand Canal d'Alsace. Parts of the abandoned line are being restored. List of canals in France
Regional council of Alsace
The Alsace Regional Council was the Conseil régional of Alsace from 1982 to 2015. As a result of reforms, the administrative région Alsace merged with two other régions to form Grand Est, effective 1 January 2016, at which point the regional councils of Alsace and Champagne-Ardenne were superseded by the Regional council of Grand Est. 27 councillors for Bas-Rhin 20 councillors for Haut-Rhin André Bord Pierre Schiélé Marcel Rudloff Adrien Zeller André Reichardt Philippe Richert
A péniche is a steel motorised inland waterway barge of up to 350 tonnes' capacity. Péniche barges were built to fit the locks of Freycinet gauge, they are visually similar to a Thames barge, but built to different specifications. The critical detail for the péniche is the dimension, 38.50m long and 5.05 m wide. They were designed for the Belgian and French canal locks, as a result of the wish to maximise space for freight, the barges tend to be flat-sided, with short, rounded bows and sterns. Nowadays the specification is still applied for commercial navigation as Class I in the Classification of European Inland Waterways; the péniche originated as a wooden vessel for inland navigation. A pointy bow was added and this version was called a'pointu' in Wallonia, a'spits' in Flanders and a'péniche flamande' in France; when ships came to be built of steel this type became a'dumb' barge that had to be towed by a towboat. In the 1910s this barge became a popular one at that. In the 1920s about 950 péniches were built in Belgium.
In the early 1940s a lot of Belgian péniches were claimed by the Germans to take part in the invasion of Great Britain. To make them seaworthy they were welded together in side by side; the last spits was built in the Netherlands in 1973. Many former freight péniches have been converted into hotel or pleasure craft; the Belgian péniche is the standard version, built for the French canal locks. Some of them have been lengthened by about 9 m or were built at 47 m or 48 m; these were constructed for transport on the Meuse river, that has larger locks between Verdun and Givet. A French péniche has less sheer than a Belgian one and a round stern with the rudder attached to the rear end rather than under the stern. After World War II a great number of them were built in Germany and sent to France as war reparation; the Dutch péniche has a a bit more sheer than the Belgian one. A wet péniche has to take on water as ballast; the full stern in the Belgian and French types, causes a higher buoyancy and not enough water around the propeller when empty.
The péniche is, because of its design, not a fast ship. A popular saying among owners is that it will hardly move forward when laden or backwards when empty. Bernard Le Sueur.
Saint-Symphorien-sur-Saône is a commune in the Côte-d'Or department in eastern France. Communes of the Côte-d'Or department INSEE
Canal de la Haute-Saône
The Canal de la Haute-Saône canal de Montbéliard à la Haute-Saône, is a canal in eastern France. Although it was designed to connect the upper course of the river Saône with the Canal du Rhône au Rhin along Lure and Ronchamp, only the short section between Allenjoie and Botans has been opened in 1923. In the section between Ronchamp and Botans, several locks and tunnels have been built, but it was never used; the section Allenjoie-Botans is 10 km long with five locks. It was closed in 2013. List of canals in France Project Babel