Surselva Surselva Region is one of the eleven administrative districts in the canton of Graubünden in Switzerland. It was created on 1 January 2017 as part of a reorganization of the canton.Graubünden,

Switzerland ). Swiss law does not designate a ''capital'' as such, but the federal parliament and government are installed in Bern, while other federal institutions, such as the federal courts, are in other cities (Bellinzona, Lausanne, Luzern, Neuchâtel ...

, source1_coordinates= , source1_elevation = , source2 = Rein Posteriur/Hinterrhein , source2_location =

Paradies Glacier The Paradies Glacier (german: Paradiesgletscher) is a 2.27 km long glacier (2007) situated in the Lepontine Alps in the canton of Graubünden in Switzerland. In 1973 it had an area of 3.99 km2. See also *List of glaciers in Switzerland ...

, Graubünden,

, source2_coordinates= , source2_elevation = , source_confluence = Reichenau , source_confluence_location =

Tamins Tamins ( rm, Tumein) is a village and a municipality in the Imboden Region in the Swiss canton of Graubünden. History Tamins is first mentioned in 1224 as ''Tuminne''. In 1225 it was mentioned as ''Tvminnis'' and in 1399 as ''Tumins''. Geogra ...

, Graubünden,

, source_confluence_coordinates= , source_confluence_elevation = , mouth =

North Sea The North Sea lies between Great Britain, Norway, Denmark, Germany, the Netherlands and Belgium. An epeiric sea on the European continental shelf, it connects to the Atlantic Ocean through the English Channel in the south and the Norwegia ...

, mouth_location =

Netherlands ) , anthem = ( en, "William of Nassau") , image_map = , map_caption = , subdivision_type = Sovereign state , subdivision_name = Kingdom of the Netherlands , established_title = Before independence , established_date = Spanish Neth ...

, mouth_coordinates = , mouth_elevation = , progression = , river_system = , basin_size = , tributaries_left = , tributaries_right = , custom_label = , custom_data = , extra = The Rhine ; french: Rhin ; nl, Rijn ; wa, Rén ; li, Rien; rm, label=

Sursilvan Sursilvan (; also ''romontsch sursilvan'' ; Sursilvan, Vallader, Surmiran, Sutsilvan, and Rumantsch Grischun: ''sursilvan''; Puter: ''sursilvaun'') is a group of dialects of the Romansh language spoken in the Swiss district of Surselva. It is ...

, Rein, rm, label=

Sutsilvan Romansh (; sometimes also spelled Romansch and Rumantsch; Sursilvan: ; Vallader, Surmiran, and Rumantsch Grischun: ; Putèr: ; Sutsilvan: , , ; Jauer: ) is a Gallo-Romance language spoken predominantly in the Swiss canton of the Grisons ( ...

and

Surmiran Surmiran (Surmiran, Vallader, Sutsilvan, Rumantsch Grischun: ''surmiran''; Puter: ''surmiraun'') is a dialect of the Romansh language. It is spoken in Surmeir and in the Albula Valley in the Grisons Canton, in Switzerland ). Swiss la ...

, Ragn, rm, label=

Rumantsch Grischun Romansh (; sometimes also spelled Romansch and Rumantsch; Sursilvan: ; Vallader, Surmiran, and Rumantsch Grischun: ; Putèr: ; Sutsilvan: , , ; Jauer: ) is a Gallo-Romance language spoken predominantly in the Swiss canton of the Gri ...

Vallader Vallader (Vallader, Sursilvan, Puter, Surmiran, and Rumantsch Grischun: ''vallader'' ; Sutsilvan: ') is a variety of the Romansh language spoken in the Lower Engadine valley (''Engiadina Bassa'') of southeast Switzerland, between Martina ...

and Puter, Rain; it, Reno ; gsw, Rhi(n), including in Alsatian and

Low Alemannic German Low Alemannic German (german: Niederalemannisch) is a branch of Alemannic German, which is part of Upper German. Its varieties are only partly intelligible to non-Alemannic speakers. Subdivisions * Lake Constance Alemannic ( de) **Northern Vora ...

; ksh, label= Ripuarian and

Low Franconian Low Franconian, Low Frankish, NetherlandicSarah Grey Thomason, Terrence Kaufman: ''Language Contact, Creolization, and Genetic Linguistics'', University of California Press, 1991, p. 321. (Calling it "Low Frankish (or Netherlandish)".)Scott Shay ...

, Rhing; la, Rhenus ; hu, Rajna . is one of the major European rivers. The river begins in the Swiss

canton of Graubünden The Grisons () or Graubünden,Names include: *german: (Kanton) Graubünden ; * Romansh: ** rm, label= Sursilvan, (Cantun) Grischun ** rm, label= Vallader, (Chantun) Grischun ** rm, label= Puter, (Chantun) Grischun ** rm, label= Surmiran, (Ca ...

in the southeastern

Swiss Alps The Alpine region of Switzerland, conventionally referred to as the Swiss Alps (german: Schweizer Alpen, french: Alpes suisses, it, Alpi svizzere, rm, Alps svizras), represents a major natural feature of the country and is, along with the Swis ...

. It forms part of the Swiss-Liechtenstein, Swiss-Austrian, 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

where it eventually empties into the

. It drains an area of 9,973 sq km and its name derives from the Celtic ''Rēnos''. There are also two German states named after the river,

North Rhine-Westphalia North Rhine-Westphalia (german: Nordrhein-Westfalen, ; li, Noordrien-Wesfale ; nds, Noordrhien-Westfalen; ksh, Noodrhing-Wäßßfaale), commonly shortened to NRW (), is a state (''Land'') in Western Germany. With more than 18 million inhabi ...

and

Rhineland-Palatinate Rhineland-Palatinate ( , ; german: link=no, Rheinland-Pfalz ; lb, Rheinland-Pfalz ; pfl, Rhoilond-Palz) is a western state of Germany. It covers and has about 4.05 million residents. It is the ninth largest and sixth most populous of the ...

. It is the second-longest river in Central and Western Europe (after the

Danube The Danube ( ; ) is a river that was once a long-standing frontier of the Roman Empire and today connects 10 European countries, running through their territories or being a border. Originating in Germany, the Danube flows southeast for , pa ...

), at about , with an average discharge of about . The Rhine and the Danube comprised much of the

Roman Empire The Roman Empire ( la, Imperium Romanum ; grc-gre, Βασιλεία τῶν Ῥωμαίων, Basileía tôn Rhōmaíōn) was the post-Roman Republic, Republican period of ancient Rome. As a polity, it included large territorial holdings aro ...

's northern inland boundary, and the Rhine has been a vital navigable waterway bringing trade and goods deep inland since those days. The various castles and defenses built along it attest to its prominence as a waterway in the

Holy Roman Empire The Holy Roman Empire was a political entity in Western, Central, and Southern Europe that developed during the Early Middle Ages and continued until its dissolution in 1806 during the Napoleonic Wars. From the accession of Otto I in 962 un ...

. Among the largest and most important cities on the Rhine are Cologne,

Rotterdam Rotterdam ( , , , lit. ''The Dam on the River Rotte'') is the second largest city and municipality in the Netherlands. It is in the province of South Holland, part of the North Sea mouth of the Rhine–Meuse–Scheldt delta, via the ''"Ne ...

Düsseldorf Düsseldorf ( , , ; often in English sources; Low Franconian and Ripuarian: ''Düsseldörp'' ; archaic nl, Dusseldorp ) is the capital city of North Rhine-Westphalia, the most populous state of Germany. It is the second-largest city in th ...

Duisburg Duisburg () is a city in the Ruhr metropolitan area of the western German state of North Rhine-Westphalia. Lying on the confluence of the Rhine and the Ruhr rivers in the center of the Rhine-Ruhr Region, Duisburg is the 5th largest city in Nort ...

Strasbourg Strasbourg (, , ; german: Straßburg ; gsw, label= Bas Rhin Alsatian, Strossburi , gsw, label=Haut Rhin Alsatian, Strossburig ) is the prefecture and largest city of the Grand Est region of eastern France and the official seat of the Eu ...

Nijmegen Nijmegen (;; Spanish and it, Nimega. Nijmeegs: ''Nimwèège'' ) is the largest city in the Dutch province of Gelderland and tenth largest of the Netherlands as a whole, located on the Waal river close to the German border. It is about ...

, and

Basel , french: link=no, Bâlois(e), it, Basilese , neighboring_municipalities= Allschwil (BL), Hégenheim (FR-68), Binningen (BL), Birsfelden (BL), Bottmingen (BL), Huningue (FR-68), Münchenstein (BL), Muttenz (BL), Reinach (BL), Riehen (BS), ...

Name

The variants of the name of the Rhine in modern languages are all derived from the

Gaulish Gaulish was an ancient Celtic language spoken in parts of Continental Europe before and during the period of the Roman Empire. In the narrow sense, Gaulish was the language of the Celts of Gaul (now France, Luxembourg, Belgium, most of Switzerl ...

name ', which was adapted in Roman-era geography (1st century BC) as Greek ('), Latin '. The spelling with ''Rh-'' in English ''Rhine'' as well as in German ' and French ' is due to the influence of Greek orthography, while the vocalization ''-i-'' is due to the

Proto-Germanic Proto-Germanic (abbreviated PGmc; also called Common Germanic) is the reconstructed proto-language of the Germanic branch of the Indo-European languages. Proto-Germanic eventually developed from pre-Proto-Germanic into three Germanic branc ...

adoption of the Gaulish name as *'' Rīnaz'', via

Old Frankish Frankish ( reconstructed endonym: *), also known as Old Franconian or Old Frankish, was the West Germanic language spoken by the Franks from the 5th to 9th century. After the Salian Franks settled in Roman Gaul, its speakers in Picardy and ...

giving

Old English Old English (, ), or Anglo-Saxon, is the earliest recorded form of the English language, spoken in England and southern and eastern Scotland in the early Middle Ages. It was brought to Great Britain by Anglo-Saxon settlers in the mid-5th c ...

Old High German Old High German (OHG; german: Althochdeutsch (Ahd.)) is the earliest stage of the German language, conventionally covering the period from around 750 to 1050. There is no standardised or supra-regional form of German at this period, and Old Hig ...

', early

Middle Dutch Middle Dutch is a collective name for a number of closely related West Germanic dialects whose ancestor was Old Dutch. It was spoken and written between 1150 and 1500. Until the advent of Modern Dutch after 1500 or c. 1550, there was no overarch ...

(c. 1200) ' (then also spelled ' or '). The modern German diphthong ' (also used in Romansh) ' is a

Central German Central German or Middle German (german: mitteldeutsche Dialekte, mitteldeutsche Mundarten, Mitteldeutsch) is a group of High German dialects spoken from the Rhineland in the west to the former eastern territories of Germany. Central German d ...

development of the early modern period, with the Alemannic name ' keeping the older vocalism. In Alemannic, the deletion of the ending ''-n'' in pausa is a recent development; the form ' is largely preserved in Lucernese dialects. ' in Ripuarian is diphthongized, as is ' in Palatine. While Spanish has adopted the Germanic vocalism ', Italian, Occitan, and Portuguese have retained the Latin '. The Gaulish name ''Rēnos'' (

Proto-Celtic Proto-Celtic, or Common Celtic, is the ancestral proto-language of all known Celtic languages, and a descendant of Proto-Indo-European. It is not attested in writing but has been partly reconstructed through the comparative method. Proto-Celtic ...

pre-Celtic The pre-Celtic period in the prehistory of Central Europe and Western Europe occurred before the expansion of the Celts or their culture in Iron Age Europe and Anatolia (9th to 6th centuries BC), but after the emergence of the Proto-Celtic languag ...

''*Reinos'') belongs to a class of river names built from the

PIE root The roots of the reconstructed Proto-Indo-European language (PIE) are basic parts of words that carry a lexical meaning, so-called morphemes. PIE roots usually have verbal meaning like "to eat" or "to run". Roots never occurred alone in the lan ...

' "to move, flow, run", also found in other names such as the

Reno Reno ( ) is a city in the northwest section of the U.S. state of Nevada, along the Nevada-California border, about north from Lake Tahoe, known as "The Biggest Little City in the World". Known for its casino and tourism industry, Reno is the ...

in Italy. The grammatical gender of the

Celtic Celtic, Celtics or Keltic may refer to: Language and ethnicity *pertaining to Celts, a collection of Indo-European peoples in Europe and Anatolia **Celts (modern) *Celtic languages **Proto-Celtic language *Celtic music *Celtic nations Sports Foo ...

name (as well as of its Greek and Latin adaptation) is masculine, and the name remains masculine in German, Dutch, French, Spanish and Italian. The Old English river name was variously inflected as masculine or feminine; and its

Old Icelandic Old Norse, Old Nordic, or Old Scandinavian, is a stage of development of North Germanic dialects before their final divergence into separate Nordic languages. Old Norse was spoken by inhabitants of Scandinavia and their overseas settlement ...

adoption was inflected as feminine.

Geography

The length of the Rhine is conventionally measured in "Rhine-kilometers" (''Rheinkilometer''), a scale introduced in 1939 which runs from the Old Rhine Bridge at Constance (0 km) to

Hook of Holland Hook of Holland ( nl, Hoek van Holland, ) is a town in the southwestern corner of Holland, hence the name; ''hoek'' means "corner" and was the word in use before the word ''kaap'' – "cape", from Portuguese ''cabo'' – became Dutch. The English t ...

(1036.20 km). The river is significantly shortened from its natural course due to a number of canalization projects completed in the 19th and 20th century. The "total length of the Rhine", to the inclusion of

Lake Constance Lake Constance (german: Bodensee, ) refers to three bodies of water on the Rhine at the northern foot of the Alps: Upper Lake Constance (''Obersee''), Lower Lake Constance (''Untersee''), and a connecting stretch of the Rhine, called the Lake ...

and the

Alpine Rhine The Alpine Rhine Valley (german: Alpenrheintal) is a glacial alpine valley, formed by the part of the Alpine Rhine (german: Alpenrhein ) between the confluence of the Anterior Rhine and Posterior Rhine at Reichenau and the Alpine Rhine's mouth ...

is more difficult to measure objectively; it was cited as by the Dutch Rijkswaterstaat in 2010. Its course is conventionally divided as follows:

Headwaters and sources

Sources

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

. Above this point is the extensive catchment of the headwaters of the Rhine. It belongs almost exclusively to the Swiss

, ranging from

Saint-Gotthard Massif The Gotthard Massif or Saint-Gotthard Massif (german: Gotthardmassiv or ; it, Massiccio del San Gottardo; rm, Massiv dal Gottard) is a mountain range in the Alps in Switzerland, located at the border of four cantons: Valais, Ticino, Uri and Gra ...

in the west via one valley lying in Ticino and Italy in the south to the

Flüela Pass The Flüela Pass (german: Flüelapass, rm, Pass dal Flüela, elevation ) is a high mountain pass of the Swiss Alps in Graubünden. Traditionally considered the boundary between the Albula and Silvretta Alps, the pass crosses the watershed / d ...

in the east. The Rhine is one of the four major rivers taking their source in the Gotthard region, along with the

Ticino Ticino (), sometimes Tessin (), officially the Republic and Canton of Ticino or less formally the Canton of Ticino,, informally ''Canton Ticino'' ; lmo, Canton Tesin ; german: Kanton Tessin ; french: Canton du Tessin ; rm, Chantun dal Tessin . ...

, Rhône and

Reuss Reuss may refer to: * Reuss (surname) *Reuss (river) in Switzerland *Reuss (state) or Reuß, several former states or countries in present-day Germany, and the Republic of Reuss * Reuss Elder Line and Reuss Younger Line The Principality of Reus ...

. 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 The Rheinwald (from Latin ''Rheni vallis'' meaning "Rhine Valley"; Romansh: ''Valrain'') is a valley in the Canton of Grisons in Switzerland, the first section of the Hinterrhein valley. The river Hinterrhein flows through three valleys in the G ...

below the

Rheinwaldhorn The Rheinwaldhorn ( it, Adula) is the highest point in the Swiss canton of Ticino at 3,402 metres above sea level. It lies on the border between the cantons of Graubünden and Ticino, in the Adula massif, part of the St. Gotthard massif of the ...

Anterior Rhine and Posterior Rhine

The source of the river is generally considered north of '' Lai da Tuma/Tomasee'' on ''Rein Anteriur/Vorderrhein'', although its southern tributary '' Rein da Medel'' is actually longer before its confluence with the Anterior Rhine near

Disentis Disentis (German) or Mustér (, Romansh), with its official name Disentis/Mustér is a village and a municipality in the Surselva Region in the Swiss canton of Graubünden. The skiing and summer tourism resort high up in the Rhine valley is ...

. :The Anterior Rhine ( rm, Rein Anteriur, german: Vorderrhein) springs from ''Lai da Tuma/Tomasee'', near the

Oberalp Pass Oberalp Pass ( rm, Alpsu or ''Cuolm d'Ursera''; german: Oberalppass) (2044 meters above sea level) is a high mountain pass in the Swiss Alps connecting the cantons of Graubünden and Uri between Disentis/Mustér and Andermatt. Winter closure ...

and passes the impressive ''

Ruinaulta Ruinaulta is a canyon created by the Anterior Rhine by Ilanz/Glion and Reichenau in the debris of the Flims Rockslide just upstream of its confluence with the Posterior Rhine at Reichenau in the Grisons, eastern Switzerland. It is sometimes know ...

'' formed by the largest visible rock slide in the alps, the Flims Rockslide. :The Posterior Rhine ( rm, Rein Posteriur, german: Hinterrhein) starts from the

, 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, ''

Roflaschlucht The Rofla Gorge ( rm, Puntcrap, german: Roflaschlucht) is an ancient and narrow section of the river Hinterrhein/Rein Posteriur between Sufers and Andeer in the canton of Graubünden. This narrow gorge was another obstacle on the approach to the ...

'' and ''

Viamala Viamala or Via Mala ( Romansh: literally, "bad path") is a narrow gorge along the river Hinterrhein between Zillis-Reischen and Thusis in the Canton of Graubünden, Switzerland, as well as the ancient and notorious pathway which traverses t ...

'', it reaches Reichenau in

The Anterior Rhine arises from numerous source streams in the upper

Rein da Tuma The Rein da Tuma is a river in Switzerland, in the Canton of Graubünden. It rises east of the Rossbodenstock with two or three mountain streams, that flow across the Tuma Alp into the Lake Toma (German: ''Tomasee'', Romansh: ''Lai da Tuma'') ...

'', which is usually 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 Maighels (german: Maighelserrhein) is one of the main tributaries of the Rhine (see Sources of the Rhine) and is a tributary to the Rein da Curnera. The firm ''Kraftwerke Vorderrhein AG'' has built a hydropower dam creating a reser ...

'', and the '' Rein da Curnera''. The Cadlimo Valley in the

canton of Ticino Ticino (), sometimes Tessin (), officially the Republic and Canton of Ticino or less formally the Canton of Ticino,, informally ''Canton Ticino'' ; lmo, Canton Tesin ; german: Kanton Tessin ; french: Canton du Tessin ; rm, Chantun dal Tessin . ...

is drained by the ''Reno di Medel'', which crosses the geomorphologic Alpine main ridge from the south. All streams in the source area are partially, sometimes completely, 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 Piz may refer to: * Piz Gloria, a mountain-top restaurant in Switzerland * Piz Buin, a mountain * Piz Dolf, a mountain * Piz Segnas, a mountain * Piz Buin (brand), a suncream brand * Piz (river) The Piz (russian: Пизь) is a right tributary ...

of the Tödi massif of the

Glarus Alps The Glarus Alps (german: Glarner Alpen) are a mountain range in central Switzerland. They are bordered by the Uri Alps and the Schwyz Alps to the west, the Lepontine Alps to the south, the Appenzell Alps to the northeast. The eastern part of ...

at above sea level. It starts with the creek ''Aua da Russein'' (lit.: "Water of the Russein"). In its lower course, the Anterior Rhine flows through a gorge named ''

'' (Flims Rockslide). The whole stretch of the Anterior Rhine to the Alpine Rhine confluence next to Reichenau in Tamins is accompanied by a long-distance hiking trail called ''Senda Sursilvana''. The Posterior Rhine flows first east-northeast, then north. It flows through the three valleys named

Schams thumb , The Schams north of Cagliatscha_Castle.html"_;"title="Andeer.__In_the_top_left,_the_ruins_of_Cagliatscha_Castle">Andeer.__In_the_top_left,_the_ruins_of_Cagliatscha_Castle_ The_Schams_(_rm.html" ;"title="Cagliatscha_Castle_.html" ;"tit ...

and

Domleschg Domleschg is a municipality in the Viamala Region in the Swiss canton of Graubünden. On 1 January 2015 the former municipalities of Almens, Paspels, Pratval, Rodels and Tomils merged to form the new municipality of Domleschg.

Heinzenberg Heinzenberg is an '' Ortsgemeinde'' – a municipality belonging to a ''Verbandsgemeinde'', a kind of collective municipality – in the Bad Kreuznach district in Rhineland-Palatinate, Germany. It belongs to the ''Verbandsgemeinde'' Kirner Land, ...

. The valleys are separated by the

Rofla Gorge The Rofla Gorge ( rm, Puntcrap, german: Roflaschlucht) is an ancient and narrow section of the river Hinterrhein/Rein Posteriur between Sufers and Andeer in the canton of Graubünden. This narrow gorge was another obstacle on the approach to the ...

and

Gorge. Its sources are located in the

Adula Alps , topo_map= Swiss Federal Office of Topography swisstopo , photo=MonteLeone0001.jpg , photo_caption=Monte Leone , country_type= Countries , country= , subdivision1_type= Cantons, Regions , subdivision1= , parent= Western Alps , borders_o ...

(

, Rheinquellhorn, and

Güferhorn The Güferhorn is a mountain in the Lepontine Alps, located between the valleys of Vals and Hinterrhein in Graubünden. At 3,379 metres above sea level it is the highest summit of the Lepontine Alps lying east of the Rheinwaldhorn. The northe ...

). The Avers Rhine joins from the south. One of its headwaters, the ''Reno di Lei'' (stowed in the

Lago di Lei Lago di Lei is a reservoir in the Valle di Lei, powering the Hinterrhein storage power stations. The reservoir is almost entirely in Italy, but the barrage was built on territory ceded by Italy to Switzerland (municipality of Ferrera, Grisons) i ...

), is partially located in Italy. Near Sils the Posterior Rhine is joined by the Albula, from the east, from the

Albula Pass The Albula Pass ( Romansh: ''Pass d'Alvra'' or , german: Albulapass) (el. 2312 m) is a Swiss mountain pass in the canton of Graubünden. It lies at the heart of the Albula Alps, on the watershed between the Albula, tributary of the Rhine and th ...

region. The Albula draws its water mainly from the

Landwasser The Landwasser is a river in Switzerland, canton of Graubünden. Its origin was Lake Davos before this was turned into a reservoir for a power station. Nowadays it is prolonged by the creek Flüelabach at its source and changes its name near D ...

with the Dischmabach as the largest source stream, but almost as much from the Gelgia, which comes down from the

Julier Pass The Julier Pass ( Romansh: ''Pass dal Güglia'', German: ''Julierpass'', Italian ''Passo del Giulia'') (el. 2284 m) is a mountain pass in Switzerland, in the Albula Alps. It connects the Engadin valley with central Graubünden, the nearest inh ...

. Numerous larger and smaller tributary rivers bear the name of the ''Rhine'' or equivalent in various Romansh idioms like ''Rein'' or ''Ragn''. Examples: * Anterior Rhine area: ''Rein Anteriur/Vorderrhein'', '' Rein da Medel'', ''

'', '' Rein da Curnera'', ''

'', ''Rein da Cristallina'', ''Rein da Nalps'', ''Rein da Plattas'', ''Rein da Sumvitg'', ''Rein da Vigliuts'', ''

Valser Rhine The Valser Rhine (german: Valser Rhein) is a source of the river Rhine in the Swiss canton of Graubünden. The river originates from the Länta Glacier and the Grauhorn Glacier at the northern foot of the Rheinwaldhorn and initially flows thro ...

'' * Posterior Rhine basin: ''Rein Posteriur/Hinterrhein'', '' Reno di Lei'', ''Madrischer Rhein'', '' Avers Rhine'', ''Jufer Rhein'' * Albula-Landwasser area: In the Dischma valley, near Davos, far east of the Rhine, there's a place called ''Am Rin'' ("Upon Rhine"). A tributary of the Dischma is called ''Riner Tälli''. Nearby, on the other side of the

Sertig The Sertig Valley is located in the municipality of Davos, south of the town, in the Swiss canton of Graubünden. It is a lateral valley of the Landwasser The Landwasser is a river in Switzerland, canton of Graubünden. Its origin was Lake Dav ...

, is the ''Rinerhorn''.

Alpine Rhine

Next to Reichenau in

the

Anterior Rhine The Vorderrhein ( German; English: ''Anterior Rhine''; Sursilvan: ; Sutsilvan: ''Ragn Anteriur''; Rumantsch Grischun, Vallader, and Puter: ''Rain Anteriur''; Surmiran: ''Ragn anteriour'') is one of the two sources of the Rhine. Its catchment a ...

and the

Posterior Rhine The Hinterrhein ( German; Italian: ''Reno Posteriore''; Sutsilvan: ''Ragn Posteriur''; Sursilvan: ''Rein Posteriur''; Rumantsch Grischun, Vallader, and Puter: ''Rain Posteriur''; Surmiran: ''Ragn posteriour''; en, Posterior Rhine) is one of ...

join and form the Alpine Rhine. The river makes a distinctive turn to the north near

Chur , neighboring_municipalities= Arosa, Churwalden, Tschiertschen-Praden, Domat/Ems, Felsberg, Malix, Trimmis, Untervaz, Pfäfers , twintowns = Bad Homburg (Germany), Cabourg (France), Mayrhofen (Austria), Mondorf-les-Bains (Luxembour ...

. This section is nearly 86 km long, and descends from a height of 599 meters to 396 meters. It flows through a wide glacial Alpine valley known as the Rhine Valley (german: Rheintal). Near

Sargans Sargans is a municipality in the ''Wahlkreis'' (constituency) of Sarganserland in the canton of St. Gallen in Switzerland. Sargans is known for its castle, which dates from before the founding of the Swiss Confederation in 1291. Sargans was ...

a natural dam, only a few meters high, prevents it from flowing into the open

Seeztal {{coord, 47.08, N, 9.37, E, display=title The Seeztal (or Seez Valley) is a valley of the canton of St. Gallen, Switzerland, extending to the east of Lake Walen for some 10 km, formed by the river Seez. The valley appears to be a left branc ...

valley and then through

Lake Walen The Walensee, also known as ''Lake Walen'' or ''Lake Walenstadt'' from Walenstadt, is one of the larger lakes in Switzerland, with about two thirds of its area in the Canton of St. Gallen and about one third in the Canton of Glarus. Other town ...

and

Lake Zurich __NOTOC__ Lake Zurich (Swiss German/ Alemannic: ''Zürisee''; German: ''Zürichsee''; rm, Lai da Turitg) is a lake in Switzerland, extending southeast of the city of Zürich. Depending on the context, Lake Zurich or ''Zürichsee'' can be used t ...

into the

Aare The Aare () or Aar () is a tributary of the High Rhine and the longest river that both rises and ends entirely within Switzerland. Its total length from its source to its junction with the Rhine comprises about , during which distance it descend ...

. The Alpine Rhine begins in the westernmost part of the Swiss canton of Graubünden, and later forms the border between Switzerland to the west and Liechtenstein and later Austria to the east. As an effect of human work, it empties into

on Austrian territory and not on the border that follows its old natural river bed. The mouth of the Rhine into Lake Constance forms an

inland delta A river delta is a landform shaped like a triangle, created by deposition of sediment that is carried by a river and enters slower-moving or stagnant water. This occurs where a river enters an ocean, sea, estuary, lake, reservoir, or (more rar ...

. The delta is delimited in the west by the ''

Alter Rhein The Alter Rhein (German for ''Old Rhine'') is the old river bed of the Alpine Rhine in St. Gallen and Vorarlberg in the Alpine Rhine Valley, which was cut off when the Rhine was straightened during the 20th century. These cut-off arms have bec ...

'' ("Old Rhine") and in the east by a modern canalized section. Most of the delta is a

nature reserve A nature reserve (also known as a wildlife refuge, wildlife sanctuary, biosphere reserve or bioreserve, natural or nature preserve, or nature conservation area) is a protected area of importance for flora, fauna, or features of geological or o ...

and

bird sanctuary An animal sanctuary is a facility where animals are brought to live and to be protected for the rest of their lives. Pattrice Jones, co-founder of VINE Sanctuary defines an animal sanctuary as "a safe-enough place or relationship within the cont ...

. It includes the Austrian towns of Gaißau, Höchst and Fußach. The natural Rhine originally branched into at least two arms and formed small islands by precipitating sediments. In the local Alemannic dialect, the singular is pronounced "Isel" and this is also the local pronunciation of ''Esel'' ("

Donkey The domestic donkey is a hoofed mammal in the family Equidae, the same family as the horse. It derives from the African wild ass, ''Equus africanus'', and may be classified either as a subspecies thereof, ''Equus africanus asinus'', or as a ...

"). Many local fields have an official name containing this element. Aerial image of the mouth of the Rhine into Lake Constance

A regulation of the Rhine was called for, with an upper canal near

Diepoldsau Diepoldsau is a municipality in the ''Wahlkreis'' (constituency) of Rheintal in the canton of St. Gallen in Switzerland. History Diepoldsau is first mentioned in 891 as ''Thiotpoldesouua''. Schmitter is first mentioned in 1385. It was the cros ...

and a lower canal at Fußach, in order to counteract the constant flooding and strong

sedimentation Sedimentation is the deposition of sediments. It takes place when particles in suspension settle out of the fluid in which they are entrained and come to rest against a barrier. This is due to their motion through the fluid in response to the ...

in the western Rhine Delta. The

Dornbirner Ach The Dornbirner Ach (also called ''Dornbirner Ache'') is a stream in Vorarlberg, Austria, with its source in the mountains near the alpine village (belongs to Dornbirn). It flows through one of the largest and most gorgeous gorges in Central Europ ...

had to be diverted, too, and it now flows parallel to the canalized Rhine into the lake. Its water has a darker color than the Rhine; the latter's lighter suspended load comes from higher up the mountains. It is expected that the continuous input of sediment into the lake will silt up the lake. This has already happened to the former Lake Tuggenersee. The cut-off Old Rhine at first formed a

swamp A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in ...

landscape. Later an artificial ditch of about two km was dug. It was made navigable to the Swiss town of Rheineck.

Lake Constance

Lake Constance consists of three bodies of water: the Obersee ("upper lake"), the Untersee ("lower lake"), and a connecting stretch of the Rhine, called the Seerhein ("Lake Rhine"). The lake is situated in Germany, Switzerland and

Austria Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous c ...

near the Alps. Specifically, its shorelines lie in the German states of

Bavaria Bavaria ( ; ), officially the Free State of Bavaria (german: Freistaat Bayern, link=no ), is a state in the south-east of Germany. With an area of , Bavaria is the largest German state by land area, comprising roughly a fifth of the total lan ...

and

Baden-Württemberg Baden-Württemberg (; ), commonly shortened to BW or BaWü, is a German state () in Southwest Germany, east of the Rhine, which forms the southern part of Germany's western border with France. With more than 11.07 million inhabitants across a ...

, the Austrian state of

Vorarlberg Vorarlberg ( , ; gsw, label= Vorarlbergisch, Vorarlbearg, , or ) is the westernmost state () of Austria. It has the second-smallest geographical area after Vienna and, although it also has the second-smallest population, it is the state with the ...

, and the Swiss cantons of

Thurgau Thurgau (; french: Thurgovie; it, Turgovia), anglicized as Thurgovia, more formally the Canton of Thurgau, is one of the 26 cantons forming the Swiss Confederation. It is composed of five districts and its capital is Frauenfeld. Thurgau is part ...

and

St. Gallen St. Gallen or traditionally St Gall, in German; it, San Gallo; rm, Son Gagl) is a Swiss city and the capital of the canton of St. Gallen. It evolved from the hermitage of Saint Gall, founded in the 7th century. Today, it is a ...

. The Rhine flows into it from the south following the Swiss-Austrian border. It is located at approximately .

Obersee

The flow of cold, grey mountain water continues for some distance into the lake. The cold water flows near the surface and at first doesn't mix with the warmer, green waters of Upper Lake. But then, at the so-called ''Rheinbrech'', the Rhine water abruptly falls into the depths because of the greater density of cold water. The flow reappears on the surface at the northern (German) shore of the lake, off the island of

Lindau Lindau (german: Lindau (Bodensee), ''Lindau am Bodensee''; ; Low Alemannic: ''Lindou'') is a major town and island on the eastern side of Lake Constance (''Bodensee'' in German) in Bavaria, Germany. It is the capital of the county (''Landkreis ...

. The water then follows the northern shore until Hagnau am Bodensee. A small fraction of the flow is diverted off the island of

Mainau Mainau also referred to as Mav(e)no(w), Maienowe (in 1242), Maienow (in 1357), Maienau, Mainowe (in 1394) and Mainaw (in 1580) is an island in Lake Constance (on the Southern shore of the Überlinger See near the city of Konstanz, Baden-Wü ...

into Lake Überlingen. Most of the water flows via the ''Constance hopper'' into the ''Rheinrinne'' ("Rhine Gutter") and Seerhein. Depending on the water level, this flow of the Rhine water is clearly visible along the entire length of the lake. The Rhine carries very large amounts of debris into the lake. In the mouth region, it is therefore necessary to permanently remove gravel by dredging. The large

sediment Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand a ...

loads are partly due to the extensive land improvements upstream. Three countries border the Obersee, namely Switzerland in the south, Austria in the southeast and the German states of

in the northeast and

in the north and northwest.

Seerhein

The Seerhein is only long. It connects the Obersee with the 30 cm lower Untersee. Distance markers along the Rhine measure the distance from the bridge in the old city center of Constance. For most of its length, the Seerhein forms the border between Germany and Switzerland. The exception is the old city center of Constance, on the Swiss side of the river. The Seerhein emerged in the last thousands of years, when erosion caused the lake level to be lowered by about 10 meters. Previously, the two lakes formed a single lake, as the name still suggests.

Untersee

Like in the Obersee, the flow the Rhine can be traced in the Untersee. Here, too, the river water is hardly mixed with the lake water. The northern parts of the Untersee (Lake Zell and Gnadensee) remain virtually unaffected by the flow. The river traverses the southern, which, in isolation, is sometimes called ''Rhinesee'' ("Lake Rhine"). The

Radolfzeller Aach The Radolfzeller Aach (also known as Hegauer Aach) is a right or north tributary of the Rhine in the south of Baden-Württemberg ( Germany). It is approximately 32 km long. Course The source of the river is the ''Aachtopf'' in Aach, the l ...

adds large amounts of water from the

system to the Untersee. Reichenau Island was formed at the same time as the Seerhein, when the water level fell to its current level. Lake Untersee is part of the border between Switzerland and Germany, with Germany on the north bank and Switzerland on the south, except both sides are Swiss in

Stein am Rhein Stein am Rhein (abbreviated as Stein a. R.) is a historic town and a municipality in the canton of Schaffhausen in Switzerland. The town's medieval centre retains the ancient street plan. The site of the city wall, and the city gates are preserve ...

, where the

High Rhine The High Rhine (german: Hochrhein) is the name used for the part of the Rhine that flows westbound from Lake Constance to Basel. The High Rhine begins at the outflow of the Rhine from the Untersee in Stein am Rhein and turns into the Upper Rhine ...

flows out of the lake.

High Rhine

Rheinfall mit Rheinfallbrücke und Schloss Laufen

The Rhine emerges from Lake Constance, flows generally westward, as the ''Hochrhein'', passes the

Rhine Falls , photo = File:SBB RABe 514 DTZ Rheinfall.jpg , photo_width = 280 , photo_caption = Rhine Falls with Rheinfall Bridge and Laufen Castle , location = On the border between the cantons of Schaffhausen and Zürich next to Schaffhausen, i ...

, and is joined by its major tributary, the

. The Aare more than doubles the Rhine's water discharge, to an average of nearly , and provides more than a fifth of the discharge at the Dutch border. The Aare also contains the waters from the summit of

Finsteraarhorn The Finsteraarhorn () is a mountain lying on the border between the cantons of Bern and Valais. It is the highest mountain of the Bernese Alps and the most prominent peak of Switzerland. The Finsteraarhorn is the ninth-highest mountain and t ...

, the highest point of the Rhine basin. The Rhine roughly forms the

German-Swiss border The German-speaking part of Switzerland (german: Deutschschweiz, french: Suisse alémanique, it, Svizzera tedesca, rm, Svizra tudestga) comprises about 65 percent of Switzerland (North Western Switzerland, Eastern Switzerland, Central Switze ...

from Lake Constance with the exceptions of the canton of Schaffhausen and parts of the cantons of

Zürich Zürich () is the list of cities in Switzerland, largest city in Switzerland and the capital of the canton of Zürich. It is located in north-central Switzerland, at the northwestern tip of Lake Zürich. As of January 2020, the municipality has 43 ...

and

Basel-Stadt Basel-Stadt or Basel-City (german: Kanton ; rm, Chantun Basilea-Citad; french: Canton de Bâle-Ville; it, Canton Basilea Città) is one of the 26 cantons forming the Swiss Confederation. It is composed of three municipalities with Basel as t ...

, until it turns north at the so-called

Rhine knee The Rhine knee or Rhine's knee (german: Rheinknie) is the name of several distinctive bends in the course of the river Rhine. Basel In Basel, the Rhine changes its westerly direction of flow in an angle of 90 degrees to a northerly direction, alo ...

, leaving Switzerland. The High Rhine begins in

at the western end of the Untersee. Unlike the Alpine Rhine and Upper Rhine, it flows to the west. It descends from 395 m to 252 m. Some stretches of the High Rhine between Stein am Rhein and Eglisau form the border between Switzerland on the south bank and Germany in the north. On other stretches, both sides are Swiss; in fact most of the

canton of Schaffhausen The canton of Schaffhausen, also canton of Schaffouse (german: Kanton Schaffhausen; rm, Chantun Schaffusa; french: Canton de Schaffhouse; it, Canton Sciaffusa) is the northernmost canton of Switzerland. The principal city and capital of the ca ...

is on the north bank. Between Eglisau and Basel, the High Rhine consistently forms the border. The

are situated below

Schaffhausen Schaffhausen (; gsw, Schafuuse; french: Schaffhouse; it, Sciaffusa; rm, Schaffusa; en, Shaffhouse) is a town with historic roots, a municipality in northern Switzerland, and the capital of the canton of the same name; it has an estimate ...

. With an average water flow of 373 m³/s (mean summer discharge 700 m³/s) it is the largest waterfall in Europe in terms of

potential energy In physics, potential energy is the energy held by an object because of its position relative to other objects, stresses within itself, its electric charge, or other factors. Common types of potential energy include the gravitational potentia ...

. The High Rhine is characterized by numerous dams. On the few remaining natural sections, there are still several

rapids Rapids are sections of a river where the river bed has a relatively steep gradient, causing an increase in water velocity and turbulence. Rapids are hydrological features between a ''run'' (a smoothly flowing part of a stream) and a '' cascade' ...

. Near

Koblenz Koblenz (; Moselle Franconian: ''Kowelenz''), spelled Coblenz before 1926, is a German city on the banks of the Rhine and the Moselle, a multi-nation tributary. Koblenz was established as a Roman military post by Drusus around 8 B.C. Its name ...

in the

canton of Aargau Aargau, more formally the Canton of Aargau (german: Kanton Aargau; rm, Chantun Argovia; french: Canton d'Argovie; it, Canton Argovia), is one of the 26 cantons forming the Swiss Confederation. It is composed of eleven districts and its capita ...

, the

joins the Rhine. With an average discharge of 557 m³/s, the Aare is more voluminous than the Rhine, which has an average discharge of 439 m³/s. Nevertheless, the Alpine Rhine is considered the main branch, because it is longer.

Upper Rhine

In the center of Basel, the first major city in the course of the stream, is located the "

"; this is a major bend, where the overall direction of the Rhine changes from west to north. Here the High Rhine ends. Legally, the Central Bridge is the boundary between High and Upper Rhine. The river now flows north as Upper Rhine through the

Upper Rhine Plain The Upper Rhine Plain, Rhine Rift Valley or Upper Rhine Graben ( German: ''Oberrheinische Tiefebene'', ''Oberrheinisches Tiefland'' or ''Oberrheingraben'', French: ''Vallée du Rhin'') is a major rift, about and on average , between Basel in the ...

, which is about 300 km long and up to 40 km wide. The most important tributaries in this area are the

Ill ILL may refer to: * ''I Love Lucy'', a landmark American television sitcom * Illorsuit Heliport (location identifier: ILL), a heliport in Illorsuit, Greenland * Institut Laue–Langevin, an internationally financed scientific facility * Interlibrar ...

below of Strasbourg, the

Neckar The Neckar () is a river in Germany, mainly flowing through the southwestern state of Baden-Württemberg, with a short section through Hesse. The Neckar is a major right tributary of the Rhine. Rising in the Schwarzwald-Baar-Kreis near Schwen ...

in Mannheim and the

Main Main may refer to: Geography * Main River (disambiguation) **Most commonly the Main (river) in Germany * Main, Iran, a village in Fars Province *"Spanish Main", the Caribbean coasts of mainland Spanish territories in the 16th and 17th centuries ...

across from Mainz. In Mainz, the Rhine leaves the Upper Rhine Valley and flows through the Mainz Basin. Fähre-Altrip Schiffe

The southern half of the Upper Rhine forms the

border Borders are usually defined as geographical boundaries, imposed either by features such as oceans and terrain, or by political entities such as governments, sovereign states, federated states, and other subnational entities. Political borders ca ...

between France (

Alsace Alsace (, ; ; Low Alemannic German/ gsw-FR, Elsàss ; german: Elsass ; la, Alsatia) is a cultural region and a territorial collectivity in eastern France, on the west bank of the upper Rhine next to Germany and Switzerland. In 2020, it had ...

) and Germany (Baden-Württemberg). The northern part forms the border between the German states of

in the west on the one hand, and

and

Hesse Hesse (, , ) or Hessia (, ; german: Hessen ), officially the State of Hessen (german: links=no, Land Hessen), is a state in Germany. Its capital city is Wiesbaden, and the largest urban area is Frankfurt. Two other major historic cities are Darms ...

on the other hand, in the east and north. A curiosity of this border line is that the parts of the city of

Mainz Mainz () is the capital and largest city of Rhineland-Palatinate, Germany. Mainz is on the left bank of the Rhine, opposite to the place that the Main joins the Rhine. Downstream of the confluence, the Rhine flows to the north-west, with Mainz ...

on the right bank of the Rhine were given to Hesse by the occupying forces in 1945. The Upper Rhine was a significant cultural landscape in Central Europe already in

antiquity Antiquity or Antiquities may refer to: Historical objects or periods Artifacts *Antiquities, objects or artifacts surviving from ancient cultures Eras Any period before the European Middle Ages (5th to 15th centuries) but still within the histo ...

and during the

Middle Ages In the history of Europe, the Middle Ages or medieval period lasted approximately from the late 5th to the late 15th centuries, similar to the post-classical period of global history. It began with the fall of the Western Roman Empire a ...

. Today, the Upper Rhine area hosts many important manufacturing and service industries, particularly in the centers Basel, Strasbourg and Mannheim-Ludwigshafen. Strasbourg is the seat of the

European Parliament The European Parliament (EP) is one of the legislative bodies of the European Union and one of its seven institutions. Together with the Council of the European Union (known as the Council and informally as the Council of Ministers), it adopts ...

, and so one of the three European capitals is located on the Upper Rhine. The Upper Rhine region was changed significantly by a Rhine straightening program in the 19th century. The rate of flow was increased and the ground water level fell significantly. Dead branches were removed by construction workers and the area around the river was made more habitable for humans on

flood plains A floodplain or flood plain or bottomlands is an area of land adjacent to a river which stretches from the banks of its channel to the base of the enclosing valley walls, and which experiences flooding during periods of high discharge.Gou ...

as the rate of flooding decreased sharply. On the French side, the

Grand Canal d'Alsace The Grand Canal of Alsace (, ) is a canal in eastern France, channeling the Upper Rhine river. It is 50 kilometers (about 30 miles) long between Kembs and Vogelgrun, and provides access to the region from the Rhine River, Basel in Switzerland ...

was dug, which carries a significant part of the river water, and all of the traffic. In some places, there are large compensation pools, for example, the huge ''Bassin de compensation de Plobsheim'' in Alsace. Rhein Mainzer Becken stromab von Mainz bei Eltville und Erbach vor Bingen Foto 2008 Wolfgang Pehlemann Wiesbaden IMG 0263

Rhein Mainzer Becken stromab von Mainz bei Eltville und Erbach vor Bingen Foto 2008 Wolfgang Pehlemann Wiesbaden IMG 0263

The Upper Rhine has undergone significant human change since the 19th century. While it was slightly modified during the Roman occupation, it was not until the emergence of engineers such as

Johann Gottfried Tulla Johann Gottfried Tulla (20 March 1770, in Karlsruhe – 27 March 1828, in Paris) was a German engineer who accomplished the straightening of the Rhine, improving navigation and alleviating the effects of flooding. His measures gave the Upper Rhine ...

that significant modernization efforts changed the shape of the river. Earlier work under

Frederick the Great Frederick II (german: Friedrich II.; 24 January 171217 August 1786) was King in Prussia from 1740 until 1772, and King of Prussia from 1772 until his death in 1786. His most significant accomplishments include his military successes in the Sil ...

surrounded efforts to ease shipping and construct dams to serve

coal Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead ...

transportation. Tulla is considered to have domesticated the Upper Rhine, a domestication that served goals such as reducing stagnant

bogs A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials often mosses, typically sphagnum moss. It is one of the four main types of wetlands. Other names for bogs include mire, mosses, quagmire, and muskeg; a ...

that fostered waterborne diseases, making regions more habitable for human settlement, and reduce high frequency of floods. Not long before Tulla went to work on widening and straightening the river, heavy floods caused significant loss of life. Four diplomatic treaties were signed among German state governments and French regions dealing with the changes proposed along the Rhine, one was "the Treaty for the Rectification of the Rhine flow from Neuberg to Dettenheim"(1817), which surrounded states such as Bourbon France and the Bavarian Palatinate. Loops, oxbows, branches and islands were removed along the Upper Rhine so that there would be uniformity to the river. The engineering of the Rhine was not without protest, farmers and fishermen had grave concerns about valuable fishing areas and farmland being lost. While some areas lost ground, other areas saw swamps and bogs be drained and turned into arable land. Johann Tulla had the goal of shortening and straightening the Upper Rhine. Early engineering projects the Upper Rhine also had issues, with Tulla's project at one part of the river creating rapids, after the Rhine cut down from erosion to sheer rock. Engineering along the Rhine eased flooding and made transportation along the river less cumbersome. These state projects were part of the advanced and technical progress going on in the country alongside the industrial revolution. For the German state, making the river more predictable was to ensure development projects could easily commence. The section of the Upper Rhine downstream from

is also known as the "Island Rhine". Here a number of

river island River Island is a London-based, multi-channel fashion brand, founded in 1948 by Bernard Lewis. The retailer has a presence in over 125 of worldwide markets, in stores and online. Best known for its trend focused womenswear offering, River Isla ...

s occur, locally known as "Rheinauen".

Middle Rhine

The Rhine is the longest river in Germany. It is here that the Rhine encounters some more of its main tributaries, such as the

, the

and, later, the

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 left bank tributary of the Rhine, which it joins at Koblenz. ...

, which contributes an average discharge of more than . Northeastern France drains to the Rhine via the Moselle; smaller rivers drain the

Vosges The Vosges ( , ; german: Vogesen ; Franconian and gsw, Vogese) are a range of low mountains in Eastern France, near its border with Germany. Together with the Palatine Forest to the north on the German side of the border, they form a single ...

and

Jura Mountains The Jura Mountains ( , , , ; french: Massif du Jura; german: Juragebirge; it, Massiccio del Giura, rm, Montagnas da Jura) are a sub-alpine mountain range a short distance north of the Western Alps and mainly demarcate a long part of the Frenc ...

uplands. Most of

Luxembourg Luxembourg ( ; lb, Lëtzebuerg ; french: link=no, Luxembourg; german: link=no, Luxemburg), officially the Grand Duchy of Luxembourg, ; french: link=no, Grand-Duché de Luxembourg ; german: link=no, Großherzogtum Luxemburg is a small land ...

and a very small part of Belgium also drain to the Rhine via the Moselle. As it approaches the Dutch border, the Rhine has an annual mean discharge of and an average width of . Between

Bingen am Rhein Bingen am Rhein () is a town in the Mainz-Bingen district in Rhineland-Palatinate, Germany. The settlement's original name was Bingium, a Celtic word that may have meant "hole in the rock", a description of the shoal behind the ''Mäuseturm'', ...

and

Bonn The federal city of Bonn ( lat, Bonna) is a city on the banks of the Rhine in the German state of North Rhine-Westphalia, with a population of over 300,000. About south-southeast of Cologne, Bonn is in the southernmost part of the Rhine-Ruhr ...

, the

Middle Rhine Between Bingen and Bonn, Germany, the river Rhine flows as the Middle Rhine (german: Mittelrhein) through the Rhine Gorge, a formation created by erosion, which happened at about the same rate as an uplift in the region, leaving the river ...

flows through the

Rhine Gorge The Rhine Gorge is a popular name for the Upper Middle Rhine Valley, a 65 km section of the Rhine between Koblenz and Rüdesheim in the states of Rhineland-Palatinate and Hesse in Germany. It was added to the UNESCO list of World Heritage ...

, a formation which was created by

erosion Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distin ...

. The rate of erosion equaled the uplift in the region, such that the river was left at about its original level while the surrounding lands raised. The gorge is quite deep and is the stretch of the river which is known for its many castles and vineyards. It is a UNESCO World Heritage Site (2002) and known as "the Romantic Rhine", with more than 40 castles and fortresses from the

and many quaint and lovely country villages.

The Mainz Basin ends in

; the Rhine continues as "Middle Rhine" into the

in the

Rhenish Slate Mountains The Rhenish Massif, Rhine Massif or Rhenish Uplands (german: Rheinisches Schiefergebirge, : 'Rhenish Slate Uplands') is a geologic massif in western Germany, eastern Belgium, Luxembourg and northeastern France. It is drained centrally, south to n ...

. In this sections the river falls from 77.4 m above sea level to 50.4 m. On the left, is located the mountain ranges of

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 ...

and

Eifel The Eifel (; lb, Äifel, ) is a low mountain range in western Germany and eastern Belgium. It occupies parts of southwestern North Rhine-Westphalia, northwestern Rhineland-Palatinate and the southern area of the German-speaking Community of ...

, on the right

Taunus 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 ...

and

Westerwald The Westerwald (; literally 'Western forest') is a low mountain range on the right bank of the river Rhine in the German federal states of Rhineland-Palatinate, Hesse and North Rhine-Westphalia. It is a part of the Rhenish Massif ( or Rhenish ...

. According to geologists, the characteristic narrow valley form was created by

by the river while the surrounding landscape was lifted (see

water gap A water gap is a gap that flowing water has carved through a mountain range or mountain ridge and that still carries water today. Such gaps that no longer carry water currents are called wind gaps. Water gaps and wind gaps often offer a prac ...

). Major tributaries in this section are the

Lahn The Lahn is a , right (or eastern) tributary of the Rhine in Germany. Its course passes through the federal states of North Rhine-Westphalia (23.0 km), Hesse (165.6 km), and Rhineland-Palatinate (57.0 km). It has its source in ...

and the

. They join the Rhine near

, for the right and left respectively. Almost the entire length of the Middle Rhine runs in the German state of Rhineland-Palatinate. The dominant economic sectors in the Middle Rhine area are

viniculture Viticulture (from the Latin word for ''vine'') or winegrowing (wine growing) is the cultivation and harvesting of grapes. It is a branch of the science of horticulture. While the native territory of ''Vitis vinifera'', the common grape vine, ran ...

and tourism. The

between

Rüdesheim am Rhein Rüdesheim am Rhein is a German winemaking town in the Rhine Gorge, and part of the UNESCO World Heritage Site in this region. It lies in the Rheingau-Taunus-Kreis district in the '' Regierungsbezirk'' of Darmstadt, Hessen. Known as Rüdesheim, it ...

and

is listed as a UNESCO

World Heritage Site A World Heritage Site is a landmark or area with legal protection by an international convention administered by the United Nations Educational, Scientific and Cultural Organization (UNESCO). World Heritage Sites are designated by UNESCO for h ...

. Near

Sankt Goarshausen Sankt Goarshausen (abbreviated St. Goarshausen) is a town located in the Rhein-Lahn-Kreis in Nassau on the eastern shore of the Rhine, in the section known as the Rhine Gorge, directly across the river from Sankt Goar, in the German state Rhin ...

, the Rhine flows around the famous rock

Lorelei The Lorelei ( ; ), spelled Loreley in German, is a , steep slate rock on the right bank of the River Rhine in the Rhine Gorge (or Middle Rhine) at Sankt Goarshausen in Germany, part of the Upper Middle Rhine Valley UNESCO World Heritage Site. ...

. 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.

Lower Rhine

, where the

Sieg The Sieg is a river in North Rhine-Westphalia and Rhineland-Palatinate, Germany. It is a right tributary of the Rhine. The river is named after the Sicambri. It is in length. The source is located in the Rothaargebirge mountains. From here th ...

flows into the Rhine, the Rhine enters the

North German Plain The North German Plain or Northern Lowland (german: Norddeutsches Tiefland) is one of the major geographical regions of Germany. It is the German part of the North European Plain. The region is bounded by the coasts of the North Sea and the Bal ...

and turns into the Lower Rhine. The Lower Rhine falls from 50 m to 12 m. The main tributaries on this stretch are the

Ruhr The Ruhr ( ; german: Ruhrgebiet , also ''Ruhrpott'' ), also referred to as the Ruhr area, sometimes Ruhr district, Ruhr region, or Ruhr valley, is a polycentric urban area in North Rhine-Westphalia, Germany. With a population density of 2,800/k ...

and the

Lippe Lippe () is a ''Kreis'' (district) in the east of North Rhine-Westphalia, Germany. Neighboring districts are Herford, Minden-Lübbecke, Höxter, Paderborn, Gütersloh, and district-free Bielefeld, which forms the region Ostwestfalen-Lippe. The ...

. Like the Upper Rhine, the Lower Rhine used to

meander A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank (cut bank) and deposits sediments on an inner, convex bank ...

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. The Lower Rhine flows through

. Its banks are usually heavily populated and industrialized, in particular the

agglomerations An urban area, built-up area or urban agglomeration is a human settlement with a high population density and infrastructure of built environment. Urban areas are created through urbanization and are categorized by urban morphology as cities, ...

Cologne, Düsseldorf and

Ruhr area The Ruhr ( ; german: Ruhrgebiet , also ''Ruhrpott'' ), also referred to as the Ruhr area, sometimes Ruhr district, Ruhr region, or Ruhr valley, is a polycentric urban area in North Rhine-Westphalia, Germany. With a population density of 2,800/k ...

. Here the Rhine flows through the largest conurbation in Germany, the Rhine-Ruhr region. One of the most important cities in this region is

with the largest

river port An inland port is a port on an inland waterway, such as a river, lake, or canal, which may or may not be connected to the sea. The term "inland port" is also used to refer to a dry port. Examples The United States Army Corps of Engineers pub ...

in Europe (Duisport). The region downstream of Duisburg is more agricultural. In Wesel, 30 km downstream of Duisburg, is located the western end of the second east–west shipping route, the Wesel-Datteln Canal, which runs parallel to the Lippe. Between Emmerich and

Cleves Kleve (; traditional en, Cleves ; nl, Kleef; french: Clèves; es, Cléveris; la, Clivia; Low Rhenish: ''Kleff'') is a town in the Lower Rhine region of northwestern Germany near the Dutch border and the River Rhine. From the 11th century ...

the

Emmerich Rhine Bridge The Emmerich Rhine Bridge (german: 'Rheinbrücke Emmerich') is a suspension bridge located in Emmerich am Rhein, Germany. Completed in 1965, it has a main span of , crossing the Rhine, carrying the Bundesstraße B 220, the federal highway betwe ...

, the longest suspension bridge in Germany, crosses the river. Near Krefeld, the river crosses the

Uerdingen line The Uerdingen Line (german: Ürdinger Linie, Uerdinger Linie, nl, Uerdinger linie; named after Uerdingen by Georg Wenker) is the isogloss within West Germanic languages that separates dialects which preserve the ''-k'' sound in the first perso ...

, the line which separates the areas where Low German and

High German The High German dialects (german: hochdeutsche Mundarten), or simply High German (); not to be confused with Standard High German which is commonly also called ''High German'', comprise the varieties of German spoken south of the Benrath an ...

are spoken. Until the early 1980s, industry was a major source of water pollution. Although many plants and factories can be found along the Rhine up into

, it is along the

Lower Rhine The Lower Rhine (german: Niederrhein; kilometres 660 to 1,033 of the river Rhine) flows from Bonn, Germany, to the North Sea at Hook of Holland, Netherlands (including the Nederrijn or "Nether Rhine" within the Rhine–Meuse–Scheldt delta); a ...

that the bulk of them are concentrated, as the river passes the major cities of Cologne,

and

. Duisburg is the home of Europe's largest inland port and functions as a hub to the sea ports of

, Antwerp and Amsterdam. The

, 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 Reforestation (occasionally, reafforestation) is the natural or intentional restocking of existing forests and woodlands (forestation) that have been depleted, usually through deforestation, but also after clearcutting. Management A debate ...

Slag Slag is a by-product of smelting ( pyrometallurgical) ores and used metals. Broadly, it can be classified as ferrous (by-products of processing iron and steel), ferroalloy (by-product of ferroalloy production) or non-ferrous/base metals (by-pr ...

and

brownfields In urban planning, brownfield land is any previously developed land that is not currently in use. It may be potentially contaminated, but this is not required for the area to be considered brownfield. The term is also used to describe land prev ...

. The Ruhr currently provides the region with drinking water. It contributes to the Rhine. Other rivers in the

Ruhr Area The Ruhr ( ; german: Ruhrgebiet , also ''Ruhrpott'' ), also referred to as the Ruhr area, sometimes Ruhr district, Ruhr region, or Ruhr valley, is a polycentric urban area in North Rhine-Westphalia, Germany. With a population density of 2,800/k ...

, above all, the

Emscher The Emscher () is a river, a tributary of the Rhine, that flows through the Ruhr area in North Rhine-Westphalia in western Germany. Its overall length is with an mean outflow near the mouth into the lower Rhine of . Description The Emscher h ...

, still carry a considerable degree of pollution.

Delta

Abbinden der Maas von der Waal 1904 aus Hochwasserschutzgründen

The Dutch name for Rhine is "Rijn". The Rhine turns west and enters the

, where, together with the rivers

Meuse The Meuse ( , , , ; wa, Moûze ) or Maas ( , ; li, Maos or ) is a major European river, rising in France and flowing through Belgium and the Netherlands before draining into the North Sea from the Rhine–Meuse–Scheldt delta. It has a ...

and

Scheldt The Scheldt (french: Escaut ; nl, Schelde ) is a river that flows through northern France, western Belgium, and the southwestern part of the Netherlands, with its mouth at the North Sea. Its name is derived from an adjective corresponding ...

, it forms the extensive Rhine-Meuse-Scheldt delta, with the largest

river delta A river delta is a landform shaped like a triangle, created by deposition of sediment that is carried by a river and enters slower-moving or stagnant water. This occurs where a river enters an ocean, sea, estuary, lake, reservoir, or (more rar ...

in Europe. Crossing the border into the Netherlands at Spijk, close to

and

Arnhem Arnhem ( or ; german: Arnheim; South Guelderish: ''Èrnem'') is a city and municipality situated in the eastern part of the Netherlands about 55 km south east of Utrecht. It is the capital of the province of Gelderland, located on both banks of ...

, the Rhine is at its widest, although the river then splits into three main

distributaries A distributary, or a distributary channel, is a stream that branches off and flows away from a main stream channel. Distributaries are a common feature of river deltas. The phenomenon is known as river bifurcation. The opposite of a distributary ...

: the

Waal WAAL (99.1 FM "The Whale") is a commercial radio station licensed to Binghamton, New York. It airs a classic rock radio format and is owned by Townsquare Media. WAAL is the oldest FM radio station in the Binghamton metropolitan area. It is a ...

Nederrijn 300px, Course of the Nederrijn Nederrijn (; "Lower Rhine"; not to be confused with the section called Lower Rhine further upstream) is the name of the Dutch part of the Rhine from the confluence at the town of Angeren of the cut-off Rhine bend ...

("Nether Rhine") and

IJssel The IJssel (; nds-nl, Iessel(t) ) is a Dutch distributary of the river Rhine that flows northward and ultimately discharges into the IJsselmeer (before the 1932 completion of the Afsluitdijk known as the Zuiderzee), a North Sea natural harbour. ...

. 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 The Merwede () etymology uncertain, possibly derived from the ancient Dutch ''Merwe'' or ''Merowe'', a word meaning "wide water") is the name of several connected stretches of river in the Netherlands, between the cities of Woudrichem, Dordrecht a ...

and

Nieuwe Merwede The Nieuwe Merwede (; "New Merwede") is a Dutch canal, mainly fed by the river Rhine, that was constructed in 1870 to form a branch in the Rhine–Meuse delta. It was dug along the general trajectories of a number of minor Biesbosch creeks to ...

(

De Biesbosch De Biesbosch National Park is one of the largest national parks of the Netherlands and one of the last extensive areas of freshwater tidal wetlands in Northwestern Europe. The Biesbosch ('forest of sedges' or 'rushwoods') consists of a large ...

), merging with the Meuse, through the

Hollands Diep Hollands Diep ( pre-1947 spelling: Hollandsch Diep) is a wide river in the Netherlands and an estuary of the Rhine and Meuse rivers. Through the Scheldt-Rhine Canal it connects to the Scheldt river and Antwerp. The Bergse Maas river and the N ...

and

Haringvliet The Haringvliet is a large inlet of the North Sea, in the province of South Holland in the Netherlands. It is an important estuary of the Rhine-Meuse delta. Near Numansdorp, the Hollands Diep splits into the Haringvliet and the Volkerak estu ...

estuaries An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environmen ...

, into the

. The

Beneden Merwede The Beneden Merwede () is a stretch of river in the Netherlands, mainly fed by the river Rhine. It starts as the continuation of the Boven Merwede after the branching-off of the Nieuwe Merwede ship canal. It flows from Hardinxveld-Giessendam to D ...

branches off, near

Hardinxveld-Giessendam Hardinxveld-Giessendam () is a municipality in the western Netherlands, in the province of South Holland. It is located about 10 km east of Dordrecht, on the river Beneden-Merwede. The municipality had a population of in and covers an a ...

and continues as the

Noord Noord () is a town and region in Aruba (part of the Kingdom of the Netherlands). This town is known for its low rise and high rise hotels, restaurants, beaches, malls, the California Lighthouse, and other places of attraction. Places of interes ...

, to join the Lek, near the village of

Kinderdijk Kinderdijk () is a village in the municipality of Molenlanden, in the province of South Holland, Netherlands. It is located about east of Rotterdam. Kinderdijk is situated in the Alblasserwaard polder at the confluence of the Lek and Noord ...

, to form the

Nieuwe Maas The Nieuwe Maas (; "New Meuse") is a distributary of the Rhine River, and a former distributary of the Maas River, in the Dutch province of South Holland. It runs from the confluence of the rivers Noord and Lek, and flows west through Rotterdam ...

; then flows past

and continues via

Het Scheur Het Scheur (; Dutch for "The Rip") is a branch of the Rhine-Meuse delta in South Holland, Netherlands, that flows west from the confluence of the Oude Maas and Nieuwe Maas branches past the towns of Rozenburg and Maassluis. It continues as the N ...

and the

Nieuwe Waterweg The Nieuwe Waterweg ("New Waterway") is a ship canal in the Netherlands from het Scheur (a branch of the Rhine-Meuse-Scheldt delta) west of the town of Maassluis to the North Sea at Hook of Holland: the Maasmond, where the Nieuwe Waterweg c ...

, to the North Sea. The

Oude Maas The Oude Maas (; en, Old Meuse) is a distributary of the river Rhine, and a former distributary of the river Maas, in the Dutch province of South Holland. It begins at the city of Dordrecht where the Beneden Merwede river splits into the Noord ...

branches off, near

Dordrecht Dordrecht (), historically known in English as Dordt (still colloquially used in Dutch, ) or Dort, is a city and municipality in the Western Netherlands, located in the province of South Holland. It is the province's fifth-largest city after Ro ...

, farther down rejoining the

to form

. The other third of the water flows through the

Pannerdens Kanaal The Pannerdens Kanaal (Pannerden Canal) is a canal in the Netherlands that was dredged between 1701 and 1709 to cut off a large, shallow bend of the river Rhine and so improve river traffic and water regulation. The canal, now indistinguishable fro ...

and redistributes in the IJssel and Nederrijn. The IJssel branch carries one ninth of the water flow of the ''Rhine'' north into the

IJsselmeer The IJsselmeer (; fy, Iselmar, nds-nl, Iesselmeer), also known as Lake IJssel in English, is a closed off inland bay in the central Netherlands bordering the provinces of Flevoland, North Holland and Friesland. It covers an area of with an av ...

(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 Wijk bij Duurstede () is a municipality and a city in the central Netherlands. Population centres * Cothen *Langbroek *Wijk bij Duurstede Topography ''Dutch Topographic map of the municipality of Wijk bij Duurstede, 2013.'' City The city ...

, the Nederrijn changes its name and becomes the Lek. It flows farther west, to rejoin the

into the

and to the North Sea. 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 Roman or Romans most often refers to: *Rome, the capital city of Italy *Ancient Rome, Roman civilization from 8th century BC to 5th century AD *Roman people, the people of ancient Rome *''Epistle to the Romans'', shortened to ''Romans'', a letter ...

times. Though they retained the name, these streams no longer carry water from the Rhine, but are used for draining the surrounding land and

polder A polder () is a low-lying tract of land that forms an artificial hydrological entity, enclosed by embankments known as dikes. The three types of polder are: # Land reclaimed from a body of water, such as a lake or the seabed # Flood plains s ...

s. From Wijk bij Duurstede, the old north branch of the Rhine is called

Kromme Rijn The Kromme Rijn () ("Crooked Rhine", for its many bends) is a river in the central Netherlands. In Roman times, this northernmost branch of the Rhine delta was the main distributary of this major European river. Along its banks the Romans buil ...

("Bent Rhine") past

Utrecht Utrecht ( , , ) is the fourth-largest city and a municipality of the Netherlands, capital and most populous city of the province of Utrecht. It is located in the eastern corner of the Randstad conurbation, in the very centre of mainland Nethe ...

, first

Leidse Rijn The Leidse Rijn (Dutch for "Leiden's Rhine") is a canal in the province of Utrecht, Netherlands. It was dug since the Middle Ages when the meandering old Rhine course silted up. The Leidse Rijn has a length of 13 km. Towns along the Leidse Rijn ...

("Rhine of

Leiden Leiden (; in English and archaic Dutch also Leyden) is a city and municipality in the province of South Holland, Netherlands. The municipality of Leiden has a population of 119,713, but the city forms one densely connected agglomeration with ...

") and then, Oude Rijn ("Old Rhine"). The latter flows west into a

sluice Sluice ( ) is a word for a channel controlled at its head by a movable gate which is called a sluice gate. A sluice gate is traditionally a wood or metal barrier sliding in grooves that are set in the sides of the waterway and can be considered ...

Katwijk Katwijk (), also spelled Katwyk, is a coastal municipality and town in the province of South Holland, which is situated in the mid-western part of the Netherlands. The Oude Rijn ("Old Rhine") river flows through the town and into the North Se ...

, where its waters can be discharged into the

. This branch once formed the line along which the

Limes Germanicus The (Latin for ''Germanic frontier'') is the name given in modern times to a line of frontier () fortifications that bounded the ancient Roman provinces of Germania Inferior, Germania Superior and Raetia, dividing the Roman Empire and the unsub ...

were built. During periods of lower sea levels within the various ice ages, the Rhine took a left turn, creating the

Channel River The Channel River was a prehistoric river flowing between England and France during periods of low sea level during the ice ages. Its tributaries included the river Rhine in modern-day Netherlands, the River Thames in modern-day England and other r ...

, the course of which now lies below the English Channel. The Rhine-Meuse Delta, the most important

natural region A natural region (landscape unit) is a basic geographic unit. Usually, it is a region which is distinguished by its common natural features of geography, geology, and climate. From the ecological point of view, the naturally occurring flora and f ...

of the

begins near Millingen aan de Rijn, close to the Dutch-German border with the division of the Rhine into

and

. The region between the Dutch-German border and Rotterdam, where the Waal, Lek, and Meuse run more or less parallel, is colloquially known as the "Great Rivers". Since the Rhine contributes most of the water, the shorter term ''Rhine Delta'' is commonly used. However, this name is also used for the

where the Rhine flows into

, 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

bifurcation Bifurcation or bifurcated may refer to: Science and technology * Bifurcation theory, the study of sudden changes in dynamical systems ** Bifurcation, of an incompressible flow, modeled by squeeze mapping the fluid flow * River bifurcation, the for ...

s: first, at Millingen aan de Rijn, the Rhine splits into

and

, which changes its name to

Angeren Angeren is a village in the municipality of Lingewaard, Gelderland province, Netherlands. It has a population of 2,851 (1 January 2009), and is located in the very eastern tip of the Betuwe, 2 km to the south of Huissen, between the cities o ...

, and second near

, the

branches off from the Nederrijn. This creates three main flows, two of which change names rather often. The largest and southern main branch begins as Waal and continues as

Boven Merwede The Boven Merwede () is a stretch of river in the Netherlands, mainly fed by the river Rhine. The Afgedamde Maas river joins the Waal at Woudrichem to form the Boven Merwede, which at Hardinxveld-Giessendam splits into the Beneden Merwede river ...

("Upper Merwede"),

("Lower Merwede"),

("the North"),

("New Meuse"),

("the Rip") and

("New Waterway"). The middle flow begins as

, then changes into Lek, then joins the Noord, thereby forming Nieuwe Maas. The northern flow keeps the name IJssel until it flows into Lake

. Three more flows carry significant amounts of water: the

("New Merwede"), which branches off from the southern branch where it changes from Boven to Beneden Merwede; the

("Old Meuse"), which branches off from the southern branch where it changes from Beneden Merwede into Noord, and

Dordtse Kil The Dordtse Kil ( pre-1947 spelling: Dordtsche Kil) is a short river in South Holland in the Netherlands. The river is tidal and forms the connection between the Oude Maas river and the Hollands Diep. The river is for most part artificial in origi ...

, which branches off from Oude Maas. Before the St. Elizabeth's flood (1421), the

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 1421 to 1904, the Meuse and Waal merged further upstream at

Gorinchem Gorinchem ( or ), also spelled Gorkum, is a city and municipality in the western Netherlands, in the province of South Holland. The municipality covers an area of of which is water. It had a population of in . The municipality of Gorinchem al ...

to form

. For flood protection reasons, the Meuse was separated from the Waal through a lock and diverted into a new outlet called "

Bergse Maas The Bergse Maas (; pre-1947 spelling: Bergsche Maas) is a canal that was constructed in 1904 to be a branch of the river Maas (French: Meuse) in the Dutch province of North Brabant. The Maas splits near Heusden into the Afgedamde Maas and the B ...

", then

Amer Amer may refer to: Places * Amer (river), a river in the Dutch province of North Brabant * Amer, Girona, a municipality in the province of Girona in Catalonia, Spain * Amber, India (also known as Amer, India), former city of Rajasthan state ** ...

and then flows into the former bay Hollands Diep. The northwestern part of the estuary (around

), 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 The Hollandse (or Hollandsche) IJssel (; "Holland IJssel", as opposed to the 'regular' or Gelderland IJssel) is a branch of the Rhine delta that flows westward from Nieuwegein on river Lek through IJsselstein, Gouda and Capelle aan den IJssel ...

Linge The Linge is a river in the Betuwe that is 99.8 km long, which makes it one of the longest rivers that flow entirely within the Netherlands. It starts near the village Doornenburg near the German border. A legend tells us that if there wi ...

, Vecht, etc.) and smaller rivers and streams. Many rivers have been closed ("dammed") and now serve as drainage channels for the numerous

polders A polder () is a low-lying tract of land that forms an artificial hydrological entity, enclosed by embankments known as dikes. The three types of polder are: # Land reclaimed from a body of water, such as a lake or the seabed # Flood plains ...

. The construction of

Delta Works The Delta Works ( nl, Deltawerken) is a series of construction projects in the southwest of the Netherlands to protect a large area of land around the Rhine–Meuse–Scheldt delta from the sea. Constructed between 1954 and 1997, the works con ...

changed the Delta in the second half of the 20th century fundamentally. Currently Rhine water runs into the sea, or into former marine bays now separated from the sea, in five places, namely at the mouths of the Nieuwe Merwede, Nieuwe Waterway (Nieuwe Maas), Dordtse Kil,

Spui A single-point urban interchange (SPUI, or ), also called a single-point interchange (SPI) or single-point diamond interchange (SPDI), is a type of highway interchange. The design was created in order to help move large volumes of traffic thro ...

and IJssel. The Rhine-Meuse Delta is a tidal delta, shaped not only by the

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 Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can ...

acts far inland. At the Waal, for example, the most landward tidal influence can be detected between

Brakel Brakel () is a municipality in the Belgian province of East Flanders in the Denderstreek and the Flemish Ardennes. The name is derived from a Carolingian villa ''Braglo'' first mentioned in 866 and located in the center of Opbrakel. Since 1970, ...

and

Zaltbommel Zaltbommel (), also known, historically and colloquially, as Bommel, is a municipality and a city in the Netherlands. History The city of Zaltbommel The town of Zaltbommel was first mentioned as "Bomela" in the year 850. Zaltbommel received ...

Geologic history

Alpine orogeny

The Rhine flows from the

Alps The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Sw ...

to the North Sea Basin. The geography and geology of its present-day watershed has been developing since the Alpine orogeny began. In southern Europe, the stage was set in the

Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period ...

Period of the

Mesozoic The Mesozoic Era ( ), also called the Age of Reptiles, the Age of Conifers, and colloquially as the Age of the Dinosaurs is the second-to-last era of Earth's geological history, lasting from about , comprising the Triassic, Jurassic and Cretace ...

Era, with the opening of the

Tethys Ocean The Tethys Ocean ( el, Τηθύς ''Tēthús''), also called the Tethys Sea or the Neo-Tethys, was a prehistoric ocean that covered most of the Earth during much of the Mesozoic Era and early Cenozoic Era, located between the ancient continents ...

, between the Eurasian and African

tectonic plates Plate tectonics (from the la, label=Late Latin, tectonicus, from the grc, τεκτονικός, lit=pertaining to building) is the generally accepted scientific theory that considers the Earth's lithosphere to comprise a number of large te ...

, between about 240 MBP and 220 MBP (million years before present). The present

Mediterranean Sea The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Western and Southern Europe and Anatolia, on the south by North Africa, and on the e ...

descends from this somewhat larger Tethys sea. At about 180 MBP, in the Jurassic Period, the two plates reversed direction and began to compress the Tethys floor, causing it to be subducted under Eurasia and pushing up the edge of the latter plate in the Alpine Orogeny of the

Oligocene The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the ...

and

Miocene The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" ...

Periods. 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 Greece,, or , romanized: ', officially the Hellenic Republic, is a country in Southeast Europe. It is situated on the southern tip of the Balkans, and is located at the crossroads of Europe, Asia, and Africa. Greece shares land borders with ...

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, highlands resulting from an earlier orogeny (

Variscan The Variscan or Hercynian orogeny was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea. Nomenclature The name ''Variscan'', come ...

) remained, such as the Ardennes,

and

. From the

Eocene The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "daw ...

onward, the ongoing Alpine orogeny caused a north–south 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

. 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

drained the northern flanks of the Alps.

Stream capture

The watershed of the Rhine reaches into the

today, but it did not start out that way.Berendsen and Stouthamer (2001) In the

period, the watershed of the Rhine reached south, only to the

and

hills, about north of the Alps. The Rhine then had the

as a tributary, but not yet the

. The northern Alps were then drained by the

. Through

stream capture Stream capture, river capture, river piracy or stream piracy is a geomorphological phenomenon occurring when a stream or river drainage system or watershed is diverted from its own bed, and flows instead down the bed of a neighbouring stream. ...

, the Rhine extended its watershed southward. By the

Pliocene The Pliocene ( ; also Pleiocene) is the epoch in the geologic time scale that extends from 5.333 million to 2.58Vosges Mountains The Vosges ( , ; german: Vogesen ; Franconian and gsw, Vogese) are a range of low mountains in Eastern France, near its border with Germany. Together with the Palatine Forest to the north on the German side of the border, they form a single ...

, including the

and the

. The northern Alps were then drained by the Rhone. By the early

Pleistocene The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in ...

period, the Rhine had captured most of its current Alpine watershed from the Rhône, including the

. Since that time, the Rhine has added the watershed above

(

Vorderrhein The Vorderrhein ( German; English: ''Anterior Rhine''; Sursilvan: ; Sutsilvan: ''Ragn Anteriur''; Rumantsch Grischun, Vallader, and Puter: ''Rain Anteriur''; Surmiran: ''Ragn anteriour'') is one of the two sources of the Rhine. Its catchment area ...

, Hinterrhein, Alpenrhein; captured from the Rhône), the upper reaches of the Main, beyond

Schweinfurt Schweinfurt ( , ; ) is a city in the district of Lower Franconia in Bavaria, Germany. It is the administrative centre of the surrounding district (''Landkreis'') of Schweinfurt and a major industrial, cultural and educational hub. The urban ag ...

and the Moselle in the Vosges Mountains, captured during the Saale Ice-age from the

, to its watershed. Around 2.5 million years ago (ending 11,600 years ago) the Ice Ages began. Since approximately 600,000 years ago, six major glacial periods have occurred, in which sea level dropped as much as and much of the continental margins were exposed. In the

Early Pleistocene The Early Pleistocene is an unofficial sub-epoch in the international geologic timescale in chronostratigraphy, being the earliest division of the Pleistocene Epoch within the ongoing Quaternary Period. It is currently estimated to span the time ...

, the Rhine followed a course to the northwest, through the present North Sea. During the so-called

Anglian glaciation The Anglian Stage is the name used in the British Isles for a middle Pleistocene glaciation. It precedes the Hoxnian Stage and follows the Cromerian Stage in the British Isles. The Anglian Stage is correlated to Marine Isotope Stage 12 (MIS 12), ...

(~450,000 yr BP, marine oxygen isotope stage 12), the northern part of the present

was blocked by the ice and a large lake developed, that overflowed through the English Channel. 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 Brest (; ) is a port city in the Finistère department, Brittany. Located in a sheltered bay not far from the western tip of the peninsula, and the western extremity of metropolitan France, Brest is an important harbour and the second French ...

and rivers, like the

River Thames The River Thames ( ), known alternatively in parts as the River Isis, is a river that flows through southern England including London. At , it is the longest river entirely in England and the second-longest in the United Kingdom, after the ...

and the

Seine ) , mouth_location = Le Havre/Honfleur , mouth_coordinates = , mouth_elevation = , progression = , river_system = Seine basin , basin_size = , tributaries_left = Yonne, Loing, Eure, Risle , tributaries ...

, 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 most recent

glacial A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate betwe ...

period ran from ~74,000 (BP = Before Present), until the end of the

(~11,600 BP). In northwest Europe, it saw two very cold phases, peaking around 70,000 BP and around 29,000–24,000 BP. The last phase slightly predates the global last ice age maximum (

Last Glacial Maximum The Last Glacial Maximum (LGM), also referred to as the Late Glacial Maximum, was the most recent time during the Last Glacial Period that ice sheets were at their greatest extent. Ice sheets covered much of Northern North America, Northern Eur ...

). 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. The English Channel, the Irish Channel and most of the

were dry land, mainly because sea level was approximately lower than today. 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. A

tundra In physical geography, tundra () is a type of biome where tree growth is hindered by frigid temperatures and short growing seasons. The term ''tundra'' comes through Russian (') from the Kildin Sámi word (') meaning "uplands", "treeless moun ...

, with Ice Age flora and fauna, stretched across middle Europe, from Asia to the Atlantic Ocean. Such was the case during the

, ca. 22,000–14,000 yr BP, when ice-sheets covered Scandinavia, the Baltics, Scotland and the Alps, but left the space between as open tundra.

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 ...

(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.

End of the last glacial period

As northwest Europe slowly began to warm up from 22,000 years ago onward, frozen

subsoil Subsoil is the layer of soil under the topsoil on the surface of the ground. Like topsoil, it is composed of a variable mixture of small particles such as sand, silt and clay, but with a much lower percentage of organic matter and humus, and it ...

and expanded

alpine glaciers A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as ...

began to thaw and fall-winter snow covers melted in spring. Much of the discharge was routed to the Rhine and its downstream extension. Rapid warming and changes of vegetation, to open forest, began about 13,000 BP. By 9000 BP, Europe was fully forested. 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 Subsidence is a general term for downward vertical movement of the Earth's surface, which can be caused by both natural processes and human activities. Subsidence involves little or no horizontal movement, which distinguishes it from slope move ...

, drowned the former coasts of Europe transgressionally. About 11000 years ago, the Rhine estuary was in the Strait of Dover. There remained some dry land in the southern

, known as

Doggerland Doggerland was an area of land, now submerged beneath the North Sea, that connected Britain to continental Europe. It was flooded by rising sea levels around 6500–6200 BCE. The flooded land is known as the Dogger Littoral. Geological sur ...

, connecting mainland Europe to Britain. About 9000 years ago, that last divide was overtopped / dissected. Man was already resident in the area when these events happened. Since 7500 years ago the situation of tides, currents and land-forms has resembled the present. Rates of

sea level rise Globally, sea levels are rising due to human-caused climate change. Between 1901 and 2018, the globally averaged sea level rose by , or 1–2 mm per year on average.IPCC, 2019Summary for Policymakers InIPCC Special Report on the Ocean and Cryo ...

dropped such that natural sedimentation by the Rhine and coastal processes widely compensate for transgression by the sea. In the southern

, due to ongoing

tectonic subsidence Tectonic subsidence is the sinking of the Earth's crust on a large scale, relative to crustal-scale features or the geoid. The movement of crustal plates and accommodation spaces created by faulting create subsidence on a large scale in a variet ...

, the coastline and sea bed are sinking at the rate of about per century (1 meter or 39 inches in last 3000 years). About 7000–5000 BP, a general warming encouraged migration of all former ice-locked areas, including up the

and down the Rhine by peoples to the east. A sudden massive expansion of the Black Sea as the

burst into it through the

Bosporus The Bosporus Strait (; grc, Βόσπορος ; tr, İstanbul Boğazı 'Istanbul strait', colloquially ''Boğaz'') or Bosphorus Strait is a natural strait and an internationally significant waterway located in Istanbul in northwestern Tu ...

may have occurred about 7500 BP.

Holocene delta

At the beginning of the Holocene (~11,700 years ago), the Rhine occupied its Late-Glacial valley. As a

ing river, it reworked its ice-age floodplain. As sea-level rise continued in the Netherlands, the formation of the Holocene Rhine-Meuse delta began (~8,000 years ago). Coeval absolute sea-level rise and

tectonic Tectonics (; ) are the processes that control the structure and properties of the Earth's crust and its evolution through time. These include the processes of mountain building, the growth and behavior of the strong, old cores of continents k ...

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 Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or ...

, as inherited from the Last Glacial period and the coastal-marine dynamics, such as barrier and tidal inlet formations. Since ~3000 yr BP (= years Before Present), human impact is seen in the delta. As a result of increasing land clearance (

Bronze Age The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second prin ...

agriculture), in the upland areas (central Germany), the sediment load of the Rhine has strongly increased and delta growth has sped up.Gouw and Erkens (2007) This has caused increased flooding and sedimentation, ending peat formation in the delta. 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). Over the past 6000 years, approximately 80 avulsions have occurred. Direct human impact in the delta began with the mining of

peat Peat (), also known as turf (), is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. The peatland ecosystem covers and is the most efficient ...

for salt and fuel from

times onward. 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 A groyne (in the U.S. groin) is a rigid hydraulic structure built perpendicularly from an ocean shore (in coastal engineering) or a river bank, interrupting water flow and limiting the movement of sediment. It is usually made out of wood, concr ...

were built to prevent the river's channels from migrating or silting up. At present, the branches Waal and Nederrijn-Lek discharge to the North Sea through the former Meuse

estuary An estuary is a partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with a free connection to the open sea. Estuaries form a transition zone between river environments and maritime environmen ...

, near Rotterdam. The river IJssel branch flows to the north and enters the

(formerly the

Zuider Zee The Zuiderzee or Zuider Zee (; old spelling ''Zuyderzee'' or ''Zuyder Zee'') was a shallow bay of the North Sea in the northwest of the Netherlands, extending about 100 km (60 miles) inland and at most 50 km (30 miles) wide, with an ...

), initially a brackish lagoon but a freshwater lake since 1932. The discharge of the Rhine is divided into three branches: the Waal (6/9 of total discharge), the Nederrijn – Lek (2/9 of total discharge) and the IJssel (1/9 of total discharge). This discharge distribution has been maintained since 1709 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

Military and cultural history

Antiquity

The Rhine was not known to

Herodotus Herodotus ( ; grc, , }; BC) was an ancient Greek historian and geographer from the Greek city of Halicarnassus, part of the Persian Empire (now Bodrum, Turkey) and a later citizen of Thurii in modern Calabria ( Italy). He is known for ha ...

and first enters the historical period in the 1st century BC in Roman-era geography. At that time, it formed the boundary between

Gaul Gaul ( la, Gallia) was a region of Western Europe first described by the Romans. It was inhabited by Celtic and Aquitani tribes, encompassing present-day France, Belgium, Luxembourg, most of Switzerland, parts of Northern Italy (only during R ...

and

Germania Germania ( ; ), also called Magna Germania (English: ''Great Germania''), Germania Libera (English: ''Free Germania''), or Germanic Barbaricum to distinguish it from the Roman province of the same name, was a large historical region in north ...

. Although it is estimated that germanic tribes have been inhabiting the area since 2000 BCE. The Upper Rhine had been part of the areal of the late

Hallstatt culture The Hallstatt culture was the predominant Western and Central European culture of Late Bronze Age (Hallstatt A, Hallstatt B) from the 12th to 8th centuries BC and Early Iron Age Europe (Hallstatt C, Hallstatt D) from the 8th to 6th centuries ...

since the 6th century BC, and by the 1st century BC, the areal of the

La Tène culture The La Tène culture (; ) was a European Iron Age culture. It developed and flourished during the late Iron Age (from about 450 BC to the Roman conquest in the 1st century BC), succeeding the early Iron Age Hallstatt culture without any defini ...

covered almost its entire length, forming a contact zone with the

Jastorf culture The Jastorf culture was an Iron Age material culture in what is now northern Germany and southern Scandinavia spanning the 6th to 1st centuries BC, forming part of the Pre-Roman Iron Age and associating with Germanic peoples. The culture ev ...

, i.e. the locus of early

- Germanic cultural contact. In Roman geography, the Rhine formed the boundary between ''Gallia'' and ''Germania'' by definition; e.g. Maurus Servius Honoratus, ''Commentary on the Aeneid of Vergil'' (8.727) ''(Rhenus) fluvius Galliae, qui Germanos a Gallia dividit'' "(The Rhine is a) river of Gaul, which divides the Germanic people from Gaul." 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 ''Res Gestae Divi Augusti'' (Eng. ''The Deeds of the Divine Augustus'') is a monumental inscription composed by the first Roman emperor, Augustus, giving a first-person record of his life and accomplishments. The ''Res Gestae'' is especially sig ...

'', a long public inscription of

Augustus Caesar Augustus (born Gaius Octavius; 23 September 63 BC – 19 August AD 14), also known as Octavian, was the first Roman emperor; he reigned from 27 BC until his death in AD 14. He is known for being the founder of the Roman Pri ...

, 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. Augustus ordered his stepson Roman general Nero Claudius Drusus, Drusus to establish 50 castra, military camps along the Rhine, starting the Germanic Wars in 12 BC. At this time, the plain of the

was the territory of the Ubii. The first urban settlement, on the grounds of what is today Downtown Cologne, along the Rhine, was ''Oppidum Ubiorum'', which was founded in 38 BC by the Ubii. Cologne became acknowledged, as a city by the Romans in AD 50, by the name of ''Colonia Claudia Ara Agrippinensium''. Castellum NigrumPullum vogelvlucht impressie Stevie Xinas 2016

Castellum NigrumPullum vogelvlucht impressie Stevie Xinas 2016

From the death of Augustus in AD 14 until after AD 70, Rome accepted as her Limes Germanicus, Germanic frontier the water-boundary of the Rhine and upper

. Beyond these rivers she held only the fertile plain of Frankfurt, opposite the Roman border fortress of Moguntiacum (

), 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. Between about AD 14 and 180, the assignment of legions was as follows: for the army of Germania Inferior, two legions at Vetera (Xanten), ''Legio I Germanica, I Germanica'' and ''Legio XX Valeria Victrix, XX Valeria'' (Pannonian troops); two legions at oppidum Ubiorum ("town of the Ubii"), which was renamed to Colonia Agrippina, descending to Cologne, ''Legio V Alaudae, V Alaudae'', a Celtic legion recruited from Gallia Narbonensis and ''Legio XXI Rapax, XXI'', possibly a Galatian legion from the other side of the empire. For the army of Germania Superior: one legion, ''Legio II Augusta, II Augusta'', at Argentoratum (

); and one, ''Legio XIII Gemina, XIII Gemina'', at Vindonissa (Windisch, Switzerland, Windisch). Vespasian had commanded II Augusta, before he became emperor. In addition, were a double legion, XIV and XVI, at Moguntiacum (

). 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 Alamanni, Alemanni. For a time, the Rhine ceased to be a border, when the Franks crossed the river and occupied Roman-dominated Celtic

, as far as Paris. Germanic tribes Crossing of the Rhine, crossed the Rhine in the Migration period, by the 5th century establishing the kingdoms of Francia on the

, Kingdom of the Burgundians, Burgundy on the Upper Rhine and Alemannia on the

. 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

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.

Medieval and modern history

By the 6th century, the Rhine was within the borders of Francia. In the 9th, it formed part of the border between Middle Francia, Middle and Western Francia, but in the 10th century, it was fully within the

, 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

on the left banks of the Upper Rhine was sold to Burgundy by Archduke Sigismund of Austria in 1469 and eventually fell to kingdom of France, France in the Thirty Years' War. The numerous historic List of castles in Rhineland-Palatinate, castles in Rhineland-Palatinate attest to the importance of the river as a commercial route. Since the Peace of Westphalia, the Upper Rhine formed a contentious border between France and Germany. Establishing "natural borders" on the Rhine was a long-term goal of French foreign policy, since the

, though the language border was – and is – far more to the west. French leaders, such as Louis XIV of France, Louis XIV and Napoleon I of France, Napoleon Bonaparte, tried with varying degrees of success to annex lands west of the Rhine. The Confederation of the Rhine was established by Napoleon, as a French client state, in 1806 and lasted until 1814, during which time it served as a significant source of resources and military manpower for the First French Empire. In 1840, the Rhine crisis, prompted by French prime minister Adolphe Thiers desire to reinstate the Rhine as a natural border, led to a diplomatic crisis and a wave of nationalism in Germany. Royal Newfoundland Regiment crossing the Rhine into Germany

Royal Newfoundland Regiment crossing the Rhine into Germany

The Rhine became an important symbol in German nationalism during the formation of the German state in the 19th century (see Rhine romanticism). * The song ''Die Wacht am Rhein'', which almost became a national anthem. * ''Das Rheingold'' – inspired by the ''Nibelungenlied'', the Rhine is one of the settings for the first opera of Richard Wagner's ''Der Ring des Nibelungen''. The action of the epic opens and ends underneath the Rhine, where three Rheinmaidens swim and protect a hoard of gold. * The Loreley/Lorelei is a rock on the eastern bank of the Rhine, that is associated with several legendary tales, poems and songs. The river spot has a reputation for being a challenge for inexperienced navigators. At the end of World War I, the Rhineland was subject to the Treaty of Versailles. This decreed that it would be occupied by the allies, until 1935 and after that, it would be a demilitarized 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 1930 and the German army re-occupied it in 1936, which was enormously popular in Germany. Although the allies could probably have prevented the reoccupation, Britain and France were not inclined to do so, a feature of their policy of appeasement to Hitler. Crossingtherhine

In World War II, it was recognized that the Rhine would present a Western Allied invasion of Germany, formidable natural obstacle to the invasion of Germany, by the Western Allies. The Rhine bridge at

, immortalized in the book, ''A Bridge Too Far (book), A Bridge Too Far'' and the A Bridge Too Far (film), film, was a central focus of the battle for Arnhem, during the failed Operation Market Garden of September 1944. The bridges at

, over the Waal distributary of the Rhine, were also an objective of Operation Market Garden. In a separate operation, the Ludendorff Bridge, crossing the Rhine at Remagen, became famous, when U.S. forces were able to capture it intact – much to their own surprise – after the Germans failed to demolish it. This also became the subject of a film, ''The Bridge at Remagen''. ''Seven Days to the River Rhine'' was a Warsaw Pact war plan for an invasion of Western Europe during the Cold War. Until 1932 the generally accepted length of the Rhine was . In 1932 the German encyclopedia Knaurs Lexikon stated the length as , 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 2010, and the Dutch Rijkswaterstaat confirms the length at .

Lists of features

Cities on the Rhine

Large cities that are situated on the Rhine: Switzerland: *

France: *

Germany: *Karlsruhe *Mannheim *Ludwigshafen *Wiesbaden *

* Cologne *Leverkusen *Neuss *

* Krefeld (Uerdingen) *

Netherlands: *

(Nederrijn) *

(Waal) *

(Kromme Rijn) *

(Nieuwe Maas) Smaller cities that are situated on the Rhine: Switzerland: *

*Kreuzlingen *

Liechtenstein: *Vaduz Germany: *Konstanz *Breisach *Speyer *Worms, Germany, Worms *

*Neuwied *Andernach *Bad Honnef *Königswinter *Niederkassel *Wesseling *Dormagen *Zons *Monheim am Rhein *Wesel *Xanten *Emmerich am Rhein Netherlands: *Zutphen (IJssel) *Deventer (IJssel) *Zwolle (IJssel) *Kampen, Overijssel, Kampen (IJssel) *

(Oude Rijn) *

(Merwede) * Wageningen (Nederrijn) * Woerden (Oude Rijn) *

( Neder Rijn / Kromme Rijn / Lek ) * Alphen aan den Rijn ( Oude Rijn )

Countries and borders

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: * the Anterior Rhine lies entirely within Switzerland, while at least one tributary to Posterior Rhine, ''Reno di Lei'' originates in Italy, but is not considered a part of the Rhine proper. * the Alpine Rhine flows within Switzerland till

, from which it becomes the border between Switzerland (to the west) and Liechtenstein (to the east) until Oberriet, and the river never flows within Liechtenstein. It then becomes the border between Switzerland (to the west) and Austria (to the east) until

where the modern and straight course enters Switzerland, while the original course ''Alter Rhein'' makes a bend to the east and continues as the Swiss-Austrian border until the confluence at Widnau. From here the river continues as the border until Lustenau, where the modern and straight course enters Austria (the only part of the river that flows within Austria), while the original course makes a bend to the west and continues as the border, until both courses enter

. * the first half of ''Seerhein'', between the upper and lower body of Lake Constance, flows within Germany (and the city of Konstanz), while the second is the German (to the north) – Swiss (to the south) frontier. * the first parts of the High Rhine, from Lake Constance to Altholz, the river alternates flowing within Switzerland and being the German-Swiss frontier (three times each). From Altholz the river is the German-Swiss border until

, where it enters Switzerland for the last time. * the Upper Rhine is the border between France (to the west) and Switzerland (to the east) for a short distance, from Basel to Hunningue. Here it becomes the Franco (to the west) – German (to the east) frontier until Au am Rhein. Hence, the main course of the Rhine never flows within France, although some river canals do. From Au am Rhein the river flows within Germany. * the Middle Rhine flows entirely within Germany. * the Lower Rhine flows within Germany until Emmerich am Rhein, where it becomes the border between The Netherlands (to the north) and Germany (to the south). At Millingen aan de Rijn the river enters the Netherlands. * all parts of the Delta Rhein flows within the Netherlands until they enter the

(

) or

(

) at the Dutch coast.

Bridges

Former distributaries

''Order: panning north to south through the Western Netherlands'': * Vecht (Utrecht) (minor channel in

times, flowing into former

lagoon) *

– Oude Rijn (Utrecht and South Holland) (main channel in Roman times, dammed in the 12th century) *

(formed after Roman times, dammed in the 13th century AD) *

(big channel in Roman times, dammed in the 14th century AD) *

-area (initiated by AD 1421–1424 storm surges and river floods, by-passed since the digging of

canal in AD 1904)

Canals

''Order: upstream to downstream'': * Rhine–Main–Danube Canal – southeastern Germany *

– eastern France * Rhine-Herne Canal – northwest Germany, connection to the Dortmund-Ems Canal and the Mittellandkanal * Maas-Waal Canal – eastcentral

* Amsterdam-Rhine Canal – central

* Scheldt-Rhine Canal – southwest

* Canal of Drusus

Notes and references

Notes

References

Bibliography

* * * * * * * * * *

External links

Rhine
with maps and details of navigation through the French section; places, ports and moorings, by the author of ''Inland Waterways of France'', Imray
Navigation details for 80 French rivers and canals
(French waterways website section)
Old maps of the Rhine
from the Eran Laor Cartographic Collection, The National Library of Israel {{Authority control Rhine, Rhine basin, International rivers of Europe Rivers of Vorarlberg Rivers of France Rivers of Liechtenstein Rivers of Switzerland Border rivers Austria–Switzerland border France–Germany border Germany–Switzerland border Graubünden–St. Gallen border Rivers of Aargau Liechtenstein–Switzerland border Geography of Central Europe Geography of Western Europe Rifts and grabens Rivers of Baden-Württemberg Rivers of North Rhine-Westphalia Rivers of Rhineland-Palatinate Federal waterways in Germany Articles containing video clips Rivers of Grand Est Rivers of Gelderland Rivers of Utrecht (province) Rivers of South Holland Rivers of Overijssel Rivers of the Netherlands Rivers of Bas-Rhin Rivers of Austria Rivers of Germany