80-636: The Fläscherberg (also known as Regitzer Spitz ) is a mountain of the Rätikon , overlooking the Rhine in the Swiss canton of Graubünden . The closest locality is Fläsch on the southern side of the mountain. At the northern foot of the mountain is the border with Liechtenstein , and the town of Balzers . This Graubünden location article is a stub . You can help Misplaced Pages by expanding it . Rhine The Rhine ( / r aɪ n / RYNE )
160-413: A domestication that served goals such as reducing stagnant bogs 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
240-684: A high degree of mutual intelligibility between these dialects. In fact, it is unclear whether the West Germanic continuum of this time period, or indeed Franconian itself, should still be considered a single language or if it should be considered a collection of similar dialects. In any case, it appears that the Frankish tribes, or the later Franks, fit primarily into the Istvaeonic dialect group, with certain Ingvaeonic influences towards
320-671: A predominantly westerly direction and flows into the Netherlands where it eventually empties into the North Sea . It drains an area of 9,973 km . Its name derives from the Celtic Rēnos . There are two German states named after the river, North Rhine-Westphalia and Rhineland-Palatinate , in addition to several districts (e.g. Rhein-Sieg ). The departments of Bas-Rhin and Haut-Rhin in Alsace (France) are also named after
400-593: A small part of northern France, and the adjoining area in Germany centered on Cologne). The Franks united as a single group under Salian Frank leadership around 500 AD. Politically, the Ripuarian Franks existed as a separate group only until about 500 AD, after which they were subsumed into the Salian Franks. The Franks were united, but the various Frankish groups must have continued to live in
480-640: A waterway in the Holy Roman Empire . Among the largest and most important cities on the Rhine are Cologne , Rotterdam , Düsseldorf , Duisburg , Strasbourg , Arnhem , and Basel . The variants of the name of the Rhine (Latin Rhenus; French Rhin, Italian Reno, Romansh Rain or Rein, Dutch Rijn, Alemannic Ry, Ripuarian Rhing) in modern languages are all derived from the Gaulish name Rēnos , which
560-747: Is a Central German development of the early modern period , with the Alemannic name R(n) keeping the older vocalism. In Alemannic, the deletion of the ending -n in pausa is a recent development; the form Rn is largely preserved in Lucernese dialects. Rhing in Ripuarian is diphthongized, as is Rhei, Rhoi in Palatine . While Spanish has adopted the Germanic vocalism Rin- , Italian, Occitan, and Portuguese have retained
640-600: Is debated whether the inscription is written in Frankish, or Old Dutch. Germanic philology and German studies have their origins in the first half of the 19th century when Romanticism and Romantic thought heavily influenced the lexicon of the linguists and philologists of the time, including pivotal figures such as the Brothers Grimm . As a result, many contemporary linguists tried to incorporate their findings in an already existing historical framework of " stem duchies " and Altstämme (lit. "old tribes", i.e.
720-428: Is difficult to determine when such a transition occurred, but it is thought to have happened by the end of the 9th century and perhaps earlier. By 900 AD the language spoken was recognizably an early form of Dutch, but that might also have been the case earlier. Old Dutch made the transition to Middle Dutch around 1150. A Dutch-French language boundary came into existence (but this was originally south of where it
800-644: Is on the sword scabbard of Bergakker which is either a direct attestation of the Old Franconian language or the earliest attestation of Old Low Franconian (Old Dutch) language. Another early sentence from the early 6th century AD (that is also described as the earliest sentence in Old Dutch as well) is found in the Lex Salica . This phrase was used to free a serf : These are the earliest sentences yet found of Old Franconian. During this early period,
880-679: Is one of the major European rivers . The river begins in the Swiss canton of Graubünden in the southeastern Swiss Alps . It forms the Swiss-Liechtenstein border and partly the Swiss-Austrian and 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
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#1732783537923960-692: Is relatively difficult for linguists today to determine what features of these dialects are due to Frankish influence, because the latter was in large part obscured, or even overwhelmed, by later developments. Most French words of Germanic origin came from Frankish, often replacing the Latin word which would have been used. It is estimated that modern French took approximately 1000 stem words from Old Franconian. Many of these words were concerned with agriculture (e.g. French : jardin 'garden'), war (e.g. French : guerre 'war') or social organization (e.g. French : baron 'baron'). Old Franconian has introduced
1040-597: Is significantly shortened from its natural course due to a number of canal projects completed in the 19th and 20th century. The "total length of the Rhine", to the inclusion of Lake Constance and the Alpine Rhine is more difficult to measure objectively; it was cited as 1,232 kilometers (766 miles) by the Dutch Rijkswaterstaat in 2010. Its course is conventionally divided as follows: The Rhine carries its name without distinctive accessories only from
1120-784: Is sometimes called Rhinesee ("Lake Rhine"). Besides the Seerhein , the Radolfzeller Aach is the main tributary of Untersee . It adds large amounts of water from the Danube system to the Untersee via the Danube Sinkhole . 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
1200-414: Is speculated that these tribes originally spoke a range of related Istvaeonic dialects in the West Germanic branch of Proto-Germanic. Sometime in the 4th or 5th centuries, it becomes appropriate to speak of Old Franconian rather than an Istvaeonic dialect of Proto-Germanic. Very little is known about what the language was like during this period. One older runic sentence (dating from around 425–450 AD)
1280-669: Is still known in some languages by terms literally meaning the " Frankish Realm ". Between the 5th and 9th centuries, Frankish spoken in Northeastern France, present-day Belgium, and the Netherlands is subsequently referred to as Old Dutch , whereas the Frankish varieties spoken in the Rhineland were heavily influenced by Elbe Germanic dialects and the Second Germanic consonant shift and would form part of
1360-643: Is the second-longest river in Central and Western Europe (after the Danube ), at about 1,230 km (760 mi), with an average discharge of about 2,900 m /s (100,000 cu ft/s). The Rhine and the Danube comprised much of the Roman Empire '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
1440-620: Is to Dutch , which is traditionally placed in the Low Franconian sub-grouping and with which it was thought to have had a common, tribal origin. In a modern linguistic context, the language of the early Franks is variously called "Old Frankish" or "Old Franconian" and refers to the language of the Franks prior to the advent of the High German consonant shift , which took place between 600 and 700 AD. After this consonant shift
1520-480: Is today). Even though living in the original territory of the Franks, these Franks seem to have broken with the endonym "Frank" around the 9th century. By this time the Frankish identity had changed from an ethnic identity to a national identity, becoming localized and confined to the modern Franconia in Germany and principally to the French province of Île-de-France . The Franks expanded south into Gaul as
1600-526: The Aare . The Aare more than doubles the Rhine's water discharge, to an average of slightly more than 1,000 m /s (35,000 cu ft/s), and provides more than a fifth of the discharge at the Dutch border. The Aare also contains the waters from the 4,274 m (14,022 ft) summit of Finsteraarhorn , the highest point of the Rhine basin . Between Eglisau and Basel , the vast majority of its length,
1680-665: The Anterior Rhine and the Posterior Rhine join and form the Alpine Rhine. The river makes a distinctive turn to the north near Chur . 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 Sargan a natural dam, only a few meters high, prevents it from flowing into
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#17327835379231760-815: The Neckar in Mannheim and the Main across from Mainz. In Mainz, the Rhine leaves the Upper Rhine Valley and flows through the Mainz Basin. The southern half of the Upper Rhine forms the border between France ( Alsace ) and Germany (Baden-Württemberg). The northern part forms the border between the German states of Rhineland-Palatinate in the west on the one hand, and Baden-Württemberg and Hesse on
1840-457: 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 Konstanz. For most of its length, the Seerhein forms the border between Germany and Switzerland. The exception is the old city center of Konstanz, on the Swiss side of the river. The Seerhein emerged in the last thousands of years, when erosion caused
1920-650: The Rhine knee , 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 , which is about 300 km long and up to 40 km wide. The most important tributaries in this area are the Ill below of Strasbourg,
2000-400: The Rhine knee , the river turns north and leaves Switzerland altogether. The High Rhine is characterized by numerous dams. On the few remaining natural sections, there are still several rapids . Over its entire course from Lake Constance to the Swiss border at Basel the river descends from 395 m to 252 m. In the center of Basel, the first major city in the course of the stream, is
2080-750: The canton of Ticino is drained by the Reno di Medel , which crosses the geomorphologic Alpine main ridge from the south. All streams in the source area are 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 of the Tödi massif of the Glarus Alps at 3,613 meters (11,854 ft) above sea level. It starts with
2160-680: The confluence of the Rein Anteriur/Vorderrhein and Rein Posteriur/Hinterrhein next to Reichenau in Tamins . Above this point is the extensive catchment area of the headwaters of the Rhine. This area belongs almost exclusively to the Swiss canton of Grisons ( Graubünden ), ranging from Saint-Gotthard Massif in the west via one valley lying in the canton of Ticino and Sondrio ( Lombardy , Italy) in
2240-490: The "people's language". Urban T. Holmes has proposed that a Germanic language continued to be spoken as a second tongue by public officials in western Austrasia and Neustria as late as the 850s, and that it completely disappeared as a spoken language from these regions only during the 10th century. The Franks also expanded their rule southeast into parts of Germany. Their language had some influence on local dialects, especially for terms relating to warfare. However, since
2320-762: The /w/ or turned it into /v/. Perhaps the best known example is the Franconian * werra ('war' < Old Northern French werre , compare Old High German werre 'quarrel'), which entered modern French as guerre and guerra in Italian , Occitan , Catalan , Spanish and Portuguese . Other examples include gant ('gauntlet', from * want ) and garder ('to guard', from * wardōn ). Franconian words starting with s before another consonant developed it into es - (e.g. Franconian skirm and Old French escremie > Old Italian scrimia > Modern French escrime ). Franconian speech habits are also responsible for
2400-443: The 19th century) bore little or limited resemblance to the actual or historical linguistic situation of the Germanic languages. Among other problems, this traditional classification of the continental West Germanic dialects can suggest stronger ties between dialects than is linguistically warranted. The Franconian group is a well known example of this, with East Franconian being much more closely related to Bavarian dialects than it
2480-516: 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 that significant modernization efforts changed the shape of the river. Earlier work under Frederick the Great surrounded efforts to ease shipping and construct dams to serve coal transportation. Tulla is considered to have domesticated the Upper Rhine,
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2560-614: The Anterior Rhine and the Rhine as a whole. The Posterior Rhine rises in the Rheinwald below the Rheinwaldhorn . The source of the river is 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 . The Anterior Rhine arises from numerous source streams in
2640-521: The Austrian state of Vorarlberg , and the Swiss cantons of Thurgau and St. Gallen . The Rhine flows into it from the south following the Swiss-Austrian border. It is located at approximately 47°39′N 9°19′E / 47.650°N 9.317°E / 47.650; 9.317 . The flow of cold, grey mountain water continues for some distance into the lake. The cold water flows near
2720-409: The Frankish dialect diverges, with the dialects which would become modern Low Franconian not undergoing the consonantal shift, while all others did so to varying degrees . As a result, the distinction between Old Dutch and Old Frankish is largely negligible, with Old Dutch (also called Old Low Franconian ) being the term used to differentiate between the affected and non-affected variants following
2800-576: The Franks remaining in the north and the rulers far to the south. Franks continued to reside in their original territories and to speak their original dialects and languages. It is not known what they called their language, but it is possible that they always called it " Diets " (i.e. "the people's language") or something similar. The word Diets is cognate with the Old English word þēodisc which, likewise, meant both nation and speech. Philologists think of Old Dutch and Old West Low Franconian as being
2880-771: The Franks were divided politically and geographically into two groups: the Salian Franks and the Ripuarian Franks . The language (or set of dialects) spoken by the Salian Franks during this period is sometimes referred to as early "Old Low Franconian", and consisted of two groups: "Old West Low Franconian" and "Old East Low Franconian". The language (or set of dialects) spoken by the Ripuarian Franks are referred to just as Old Franconian dialects (or, by some, as Old Frankish dialects). However, as already stated above, it may be more accurate to think of these dialects not as early Old Franconian but as Istvaeonic dialects in
2960-494: The Franks who had settled more to the south of this area in northern Gaul started adopting the common Latin of the local population. This Colloquial Latin language acquired the name of the people who came to speak it (Frankish or Français ); north of the French-Dutch language boundary, the language was no longer referred to as "Frankish" (if it ever was referred to as such) but rather came to be referred to as " Diets ", i.e.
3040-480: The High Rhine forms the border between Germany and Switzerland . Only for brief distances at its extremities does the river run entirely within Switzerland; at the eastern end it separates the bulk of the canton of Schaffhausen and the German exclave of Büsingen am Hochrhein on the northern bank from cantons of Zürich and Thurgau , while at the western end it bisects the canton of Basel-Stadt . Here, at
3120-663: The Latin Ren- . The Gaulish name Rēnos ( Proto-Celtic or pre-Celtic *Reinos ) belongs to a class of river names built from the PIE root *rei- "to move, flow, run", also found in other names such as the Reno in Italy. The grammatical gender of the Celtic 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
3200-875: The Posterior Rhine is joined by the Albula , from the east, from the Albula Pass region. The Albula draws its water mainly from the Landwasser with the Dischmabach as the largest source stream, but almost as much from the Gelgia , which comes down from the Julier Pass . Numerous larger and smaller tributary rivers bear the name of the Rhine or equivalent in various Romansh idioms, including Rein or Ragn , including: Next to Reichenau in Tamins
3280-453: The Rhine into Lake Constance forms an inland delta . The delta is delimited in the west by the Alter Rhein and in the east by the modern canalized section of the Alpine Rhine ( Fußacher Durchstich ). Most of the delta is a nature reserve and bird sanctuary . 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
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3360-421: The West Germanic branch of Proto-Germanic. At around the 5th century, the Franks probably spoke a range of related dialects and languages rather than a single uniform dialect or language. The language of both government and the Church was Latin. During the expansion into France and Germany, many Frankish people remained in the original core Frankish territories in the north (i.e. southern Netherlands, Flanders,
3440-406: The Western Roman Empire collapsed in the fifth century. Although the Franks would eventually conquer almost all of Gaul, speakers of Old Franconian expanded only into northern Gaul in numbers sufficient to have a linguistic effect. For several centuries, northern Gaul was a bilingual territory ( Latin and Franconian). The language used in writing, in government and by the Church was Latin. Eventually,
3520-468: The aforementioned Second Germanic consonant shift. The Germanic languages are traditionally divided into three groups: West , East and North Germanic. Their exact relation is difficult to determine, and they remained mutually intelligible throughout the Migration Period , rendering some individual varieties difficult to classify. The language spoken by the Franks was part of the West Germanic language group, which had features from Proto-Germanic in
3600-442: The area around the river was made more habitable for humans on flood plains as the rate of flooding decreased sharply. On the French side, the Grand Canal d'Alsace 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. The Upper Rhine has undergone significant human change since
3680-404: 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 landscape. Later an artificial ditch of about two km
3760-420: The centers Basel, Strasbourg and Mannheim-Ludwigshafen. Strasbourg is the seat of the European Parliament , 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
3840-603: 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
3920-457: 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 Mainz is also known as the "Island Rhine". Here a number of river islands occur, locally known as "Rheinauen". Old Frankish Frankish ( reconstructed endonym: * Frankisk ), also known as Old Franconian or Old Frankish ,
4000-415: The creek Aua da Russein (lit.: "Water of the Russein"). In its lower course, the Anterior Rhine flows through a gorge named Ruinaulta (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
4080-444: The flow is diverted off the island of Mainau 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 – over three million cubic meters (110,000,000 cu ft) annually. In
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#17327835379234160-416: 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
4240-418: The lake level to be lowered by about 10 meters. Previously, the two lakes formed a single lake, as the name still suggests. 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,
4320-416: The language of both the administration and the Church was Latin, this unification did not lead to the development of a supra-regional variety of Franconian nor a standardized German language. At the same time that the Franks were expanding southeast into what is now southern Germany, there were linguistic changes taking place in the region. The High German consonant shift (or second Germanic consonant shift )
4400-471: The late Jastorf culture (c. 1st century BC). The West Germanic group is characterized by a number of phonological and morphological innovations not found in North and East Germanic. The West Germanic varieties of the time are generally split into three dialect groups: Ingvaeonic (North Sea Germanic), Istvaeonic (Weser–Rhine Germanic) and Irminonic (Elbe Germanic). While each had its own distinct characteristics, there certainly must have still been
4480-482: The local Alemannic dialect, the singular is pronounced "Isel" and this is also the local pronunciation of Esel (" Donkey "). Many local fields have an official name containing this element. A regulation of the Rhine was called for, with an upper canal near Diepoldsau and a lower canal at Fußach, in order to counteract the constant flooding and strong sedimentation in the western Rhine Delta. The Dornbirner Ach had to be diverted, too, and it now flows parallel to
4560-410: The modern Central Franconian and Rhine Franconian dialects of German and Luxembourgish . The Old Frankish language is poorly attested and mostly reconstructed from Frankish loanwords in Old French , and inherited words in Old Dutch, as recorded in the 9th to 12th centuries. A notable exception is the Bergakker inscription , which may represent a primary record of 5th-century Frankish, though it
4640-454: The modern French word for the nation, France ( Francia ), meaning 'land of the Franks'. According to one hypothesis, the name for the Paris region, Île-de-France , was also given by the Franks. The influence of Franconian on French is decisive for the birth of the early langues d'oïl compared to the other Romance languages , that appeared later such as Occitan , Romanian , Portuguese , Spanish , Italian , etc., because its influence
4720-454: The most part did not experience the shift. The set of dialects of the Franks who continued to live in their original territory in Germany eventually developed in three different ways and eventually formed three modern branches of Franconian languages . The Frankish Empire later extended throughout neighboring France and Germany. The language of the Franks had some influence on the local languages (especially in France), but did not develop into
4800-444: The mouth region, it is therefore necessary to permanently remove gravel by dredging. The large sediment 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 Bavaria in the northeast and Baden-Württemberg in the north and northwest. The Seerhein is only 4 kilometers (2.5 mi) long. It connects
4880-459: The north bank and Switzerland on the south, except both sides are Swiss in Stein am Rhein , where the High Rhine flows out of the lake. The High Rhine ( Hochrhein ) begins in Stein am Rhein at the western end of the Untersee. Now flowing generally westwards, it passes over the Rhine Falls ( Rheinfall ) below Schaffhausen before being joined – near Koblenz in the canton of Aargau – by its major tributary,
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#17327835379234960-443: The northwest (still seen in modern Dutch), and more Irminonic (High German) influences towards the southeast. The scholarly consensus concerning the Migration Period is that the Frankish identity emerged during the first half of the 3rd century out of various earlier, smaller Germanic groups, including the Salii , Sicambri , Chamavi , Bructeri , Chatti , Chattuarii , Ampsivarii , Tencteri , Ubii , Batavi , and Tungri . It
5040-506: The open Sztal valley and then through Lake Walen and Lake Zurich into the Aare . 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 Lake Constance on Austrian territory and not on the border that follows its old natural river bed called Alter Rhein ( lit. ' Old Rhine ' ). The mouth of
5120-424: The other hand, in the east and north. A curiosity of this border line is that the parts of the city of 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 and during the Middle Ages . Today, the Upper Rhine area hosts many important manufacturing and service industries, particularly in
5200-406: The river. Some adjacent towns are named after it, such as Rheinau , Rheineck , Rheinfelden (CH) and Rheinfelden (D). The International Commission for the Hydrology of the Rhine Basin (CHR) and EUWID contend that the river could experience a massive decrease in volume, or even dry up completely in case of drought, within the next 30 to 80 years, as a result of the climate crisis . The Rhine
5280-507: The same areas that they had lived in before unification, and to speak the same dialects as before. There must have been a close relationship between the various Franconian dialects. There was also a close relationship between Old Low Franconian (i.e. Old Dutch) and its neighboring Old Saxon and Old Frisian languages and dialects to the north and northeast, as well as the related Old English (Anglo-Saxon) dialects spoken in southern and eastern Britain. A widening cultural divide grew between
5360-444: The same language. However, sometimes reference is made to a transition from the language spoken by the Salian Franks to Old Dutch . The language spoken by the Salian Franks must have developed significantly during the seven centuries from 200 to 900 AD. At some point, the language spoken by the Franks must have become identifiably Dutch. Because Franconian texts are almost non-existent and Old Dutch texts scarce and fragmentary, it
5440-402: The same ones. Below is a non-exhaustive list of French words of Frankish origin. An asterisk prefixing a term indicates a reconstructed form of the Frankish word. Most Franconian words with the phoneme w changed it to gu when entering Old French and other Romance languages ; however, the northern langues d'oil such as Picard, Norman, Walloon, Burgundian, Champenois an Lorrain retained
5520-450: The six Germanic tribes then thought to have formed the "German nation" in the traditional German nationalism of the elites) resulting in a taxonomy which spoke of " Bavarian ", " Saxon ", " Frisian ", " Thuringian ", " Swabian " and " Frankish " dialects. While this nomenclature became generally accepted in traditional Germanic philology, it has also been described as "inherently inaccurate" as these ancient ethnic boundaries (as understood in
5600-399: The south to the Flüela Pass in the east. The Rhine is one of four major rivers taking their source in the Gotthard region, along with the Ticino (drainage basin of the Po ), Rhône and Reuss (Rhine basin). The Witenwasserenstock is the triple watershed between the Rhine, Rhône and Po. Traditionally, Lake Toma near the Oberalp Pass in the Gotthard region is seen as the source of
5680-440: The standard language or lingua franca . The Franks conquered adjoining territories of Germany (including the territory of the Allemanni ). The Frankish legacy survives in these areas, for example, in the names of the city of Frankfurt and the area of Franconia . The Franks brought their language with them from their original territory and, as in France, it must have had an effect on the local dialects and languages. However, it
5760-412: The surface and at first does not 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 . The water then follows the northern shore until Hagnau am Bodensee . A small fraction of
5840-567: The three valleys named Rheinwald , Schams and Domleschg - Heinzenberg . The valleys are separated by the Rofla Gorge and Viamala Gorge. Its sources are located in the Adula Alps ( Rheinwaldhorn , Rheinquellhorn , and Güferhorn ). The Avers Rhine joins from the south. One of its headwaters, the Reno di Lei (stowed in the Lago di Lei ), is partially located in Italy. Near Sils
5920-499: The upper Surselva and flows in an easterly direction. One source is Lai da Tuma (2,345 m (7,694 ft)) with the Rein 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 , and the Rein da Curnera . The Cadlimo Valley in
6000-479: Was a phonological development ( sound change ) that took place in the southern parts of the West Germanic dialect continuum in several phases, probably beginning between the 3rd and 5th centuries AD, and was almost complete before the earliest written records in the High German language were made in the 9th century. The resulting language, Old High German , can be neatly contrasted with Low Franconian , which for
6080-1038: Was adapted in Roman-era geography (1st century BC) as Latin Rhenus , and as Greek Ῥῆνος ( Rhēnos ). The spelling with Rh- in English Rhine as well as in German Rhein and French Rhin is due to the influence of Greek orthography, while the vocalization -i- is due to the Proto-Germanic adoption of the Gaulish name as * Rīnaz , via Old Frankish giving Old English Rín , Old High German Rīn , early Middle Dutch ( c. 1200 ) Rijn (then also spelled Ryn or Rin ). The modern German diphthong Rhein (also used in Romansh ) Rein, Rain
6160-468: Was dug. It was made navigable to the Swiss town of Rheineck . 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 near the Alps. Specifically, its shorelines lie in the German states of Bavaria and Baden-Württemberg ,
6240-656: Was greater than the respective influence of Visigothic and Lombardic (both Germanic languages ) on Occitan, the Romance languages of Iberia, and Italian . Not all of these loanwords have been retained in modern French. French has also passed on words of Franconian origin to other Romance languages, and to English. Old Franconian has also left many etyma in the different northern langues d'oïl such as Burgundian , Champenois , Lorrain , Norman , Picard and Walloon , more than in Standard French, and not always
6320-675: Was the West Germanic language spoken by the Franks from the 5th to 9th century. After the Salian Franks settled in Roman Gaul (roughly, present-day France ), its speakers in Picardy and Île-de-France were outnumbered by the local populace who spoke Proto-Romance dialects. However, many modern French words and place names, including the eventual country's name, "France", have a Frankish (i.e. Germanic ) origin. France itself
6400-465: Was variously inflected as masculine or feminine; and its Old Icelandic adoption was inflected as feminine. The length of the Rhine is conventionally measured in "Rhine-kilometers" ( Rheinkilometer ), a scale introduced in 1939 which runs from the 0 km datum at Old Rhine Bridge in the city of Konstanz , at the western end of Lake Constance , to the Hook of Holland at 1,036.20 km. The river
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