80-601: Hammerstein is a municipality on the river Rhine in the district of Neuwied in Rhineland-Palatinate in Germany . This Neuwied district location article is a stub . You can help Misplaced Pages by expanding it . Rhine The Rhine ( / r aɪ n / RYNE ) is one of the major European rivers . The river begins in the Swiss canton of Graubünden in the southeastern Swiss Alps . It forms
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
240-747: 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
320-590: Is also a hundred-year "dearth of continuous texts" after the death of Notker Labeo in 1022. The mid-11th century is widely accepted as marking the transition to Middle High German . Old High German encompasses the dialects that had undergone the Second Sound Shift during the 6th century—namely all of the Upper and Central German dialects. The Franks in the western part of Francia ( Neustria and western Austrasia ) gradually adopted Gallo-Romance by
400-589: 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
480-471: Is in Modern German). The following is a sample conjugation of a strong verb, nëman "to take". Any description of OHG syntax faces a fundamental problem: texts translated from or based on a Latin original will be syntactically influenced by their source, while the verse works may show patterns that are determined by the needs of rhyme and metre, or that represent literary archaisms. Nonetheless,
560-649: 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
640-784: 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
720-506: Is the earliest stage of the German language , conventionally identified as the period from around 500/750 to 1050. Rather than representing a single supra-regional form of German, Old High German encompasses the numerous West Germanic dialects that had undergone the set of consonantal changes called the Second Sound Shift . At the start of this period, dialect areas reflected the territories of largely independent tribal kingdoms, but by 788
800-578: Is the sole survivor of what must have been a vast oral tradition. Other important works are the Evangelienbuch ( Gospel harmony ) of Otfrid von Weissenburg , the Ludwigslied and the 9th century Georgslied . The boundary to Early Middle High German (from c. 1050 ) is not clear-cut. An example of Early Middle High German literature is the Annolied . The Lord's Prayer
880-526: 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,
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#1732765671652960-660: The Abrogans , a Latin–Old High German glossary variously dated between 750 and 780, probably from Reichenau . The 8th century Merseburg Incantations are the only remnant of pre-Christian German literature. The earliest texts not dependent on Latin originals would seem to be the Hildebrandslied and the Wessobrunn Prayer , both recorded in manuscripts of the early 9th century, though the texts are assumed to derive from earlier copies. The Bavarian Muspilli
1040-665: 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
1120-706: The Carolingian Renaissance in the 9th. The dedication to the preservation of Old High German epic poetry among the scholars of the Carolingian Renaissance was significantly greater than could be suspected from the meagre survivals we have today (less than 200 lines in total between the Hildebrandslied and the Muspilli ). Einhard tells how Charlemagne himself ordered that the epic lays should be collected for posterity. It
1200-548: The Middle High German forms of words, particularly with respect to the consonants. Old High German had six phonemic short vowels and five phonemic long vowels. Both occurred in stressed and unstressed syllables. In addition, there were six diphthongs. Notes: By the mid 11th century the many different vowels found in unstressed syllables had almost all been reduced to ⟨e⟩ / ə / . Examples: (The New High German forms of these words are broadly
1280-815: 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
1360-457: 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
1440-701: 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,
1520-400: 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
1600-750: 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
1680-680: 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
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#17327656716521760-533: The (Latin) text or other aid to the reader. Old High German is generally dated from around 750 to around 1050. The start of this period sees the beginning of the OHG written tradition, at first with only glosses, but with substantial translations and original compositions by the 9th century. However, the fact that the defining feature of Old High German, the Second Sound Shift, may have started as early as
1840-516: 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,
1920-431: The 6th century and is complete by 750, means that some take the 6th century to be the start of the period. Alternatively, terms such as Voralthochdeutsch ("pre-OHG") or vorliterarisches Althochdeutsch ("pre-literary OHG") are sometimes used for the period before 750. Regardless of terminology, all recognize a distinction between a pre-literary period and the start of a continuous tradition of written texts around
2000-614: 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
2080-521: 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
2160-720: The Biblical texts were translated from Greek, not Latin) raise the possibility that it was an independent development. Germanic also had no future tense, but again OHG created periphrastic forms, using an auxiliary verb skulan (Modern German sollen ) and the infinitive, or werden and the present participle: Thu scalt beran einan alawaltenden (Otfrid's Evangelienbuch I, 5,23) "You shall bear an almighty one" Inti nu uuirdist thu suigenti' (Tatian 2,9) "And now you will start to fall silent" Latin: Et ecce eris tacens (Luke 1:20) The present tense continued to be used alongside these new forms to indicate future time (as it still
2240-536: 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 the river. Some adjacent towns are named after it, such as Rheinau , Rheineck , Rheinfelden (CH) and Rheinfelden (D). The International Commission for
2320-643: 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 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
2400-480: 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
2480-636: 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 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
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2560-468: The Late OHG changes that affected Middle High German : Germanic had a simple two-tense system, with forms for a present and preterite . These were inherited by Old High German, but in addition OHG developed three periphrastic tenses : the perfect , pluperfect and future . The periphrastic past tenses were formed by combining the present or preterite of an auxiliary verb ( wësan , habēn ) with
2640-663: 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
2720-692: The OHG Isidor or Notker show a similar awareness. The charts show the vowel and consonant systems of the East Franconian dialect in the 9th century. This is the dialect of the monastery of Fulda , and specifically of the Old High German Tatian . Dictionaries and grammars of OHG often use the spellings of the Tatian as a substitute for genuine standardised spellings, and these have the advantage of being recognizably close to
2800-875: 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
2880-512: 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
2960-893: 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 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
3040-406: The administration and the Church was Latin, and this unification did not therefore lead to any development of a supra-regional variety of Frankish nor a standardized Old High German; the individual dialects retained their identity. There was no standard or supra-regional variety of Old High German—every text is written in a particular dialect, or in some cases a mixture of dialects. Broadly speaking,
3120-424: The almighty father"). By the end of the OHG period, however, use of a subject pronoun has become obligatory, while the definite article has developed from the original demonstrative pronoun ( der, diu, daz ) and the numeral ein ("one") has come into use as an indefinite article. These developments are generally seen as mechanisms to compensate for the loss of morphological distinctions which resulted from
3200-442: 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
3280-445: The basic word order rules are broadly those of Modern Standard German . Two differences from the modern language are the possibility of omitting a subject pronoun and lack of definite and indefinite articles . Both features are exemplified in the start of the 8th century Alemannic creed from St Gall : kilaubu in got vater almahticun (Modern German, Ich glaube an Gott den allmächtigen Vater ; English "I believe in God
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3360-443: The beginning of the OHG period, with the linguistic boundary later stabilised approximately along the course of the Meuse and Moselle in the east, and the northern boundary probably a little further south than the current boundary between French and Dutch . North of this line, the Franks retained their language, but it was not affected by the Second Sound Shift, which thus separated the Low Franconian or Old Dutch varieties from
3440-404: 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
3520-420: 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
3600-603: 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
3680-443: The conquests of Charlemagne had brought all OHG dialect areas into a single polity . The period also saw the development of a stable linguistic border between German and Gallo-Romance , later French . Old High German largely preserved the synthetic inflectional system inherited from its ancestral Germanic forms. The eventual disruption of these patterns, which led to the more analytic grammar, are generally considered to mark
3760-424: 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 High German Old High German ( OHG ; German : Althochdeutsch (Ahdt., Ahd.) )
3840-415: 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
3920-413: The end of the OHG period. At the beginning of the period, no Germanic language was spoken east of a line from Kieler Förde to the rivers Elbe and Saale , earlier Germanic speakers in the Northern part of the area having been displaced by the Slavs . This area did not become German-speaking until the German eastward expansion ("Ostkolonisation", "Ostsiedlung") of the early 12th century, though there
4000-490: The end of the Old High German period, Notker Labeo was among the greatest stylists in the language, and developed a systematic orthography. Old High German marked the culmination of a shift away from runic writing of the pre-OHG period to Latin alphabet . This shift led to considerable variations in spelling conventions, as individual scribes and scriptoria had to develop their own transliteration of sounds not native to Latin script . Otfrid von Weissenburg , in one of
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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#17327656716524160-416: 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,
4320-437: The language by the 8th century, others exclude Langobardic from discussion of OHG. As Heidermanns observes, this exclusion is based solely on the external circumstances of preservation and not on the internal features of the language. The end of the period is less controversial. The sound changes reflected in spelling during the 11th century led to the remodelling of the entire system of noun and adjective declensions . There
4400-422: The language of the Carolingian court or that it is attested in the Ludwigslied , whose presence in a French manuscript suggests bilingualism , are controversial. Old High German literacy is a product of the monasteries, notably at St. Gallen , Reichenau Island and Fulda . Its origins lie in the establishment of the German church by Saint Boniface in the mid-8th century, and it was further encouraged during
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
4560-418: The main dialect divisions of Old High German seem to have been similar to those of later periods—they are based on established territorial groupings and the effects of the Second Sound Shift, which have remained influential until the present day. But because the direct evidence for Old High German consists solely of manuscripts produced in a few major ecclesiastical centres, there is no isogloss information of
4640-411: The majority of Old High German texts are religious in nature and show strong influence of ecclesiastical Latin on the vocabulary. In fact, most surviving prose texts are translations of Latin originals. Even secular works such as the Hildebrandslied are often preserved only because they were written on spare sheets in religious codices . The earliest Old High German text is generally taken to be
4720-422: The middle of the 8th century. Differing approaches are taken, too, to the position of Langobardic . Langobardic is an Elbe Germanic and thus Upper German dialect, and it shows early evidence for the Second Sound Shift. For this reason, some scholars treat Langobardic as part of Old High German, but with no surviving texts — just individual words and names in Latin texts — and the speakers starting to abandon
4800-413: The more easterly Franconian dialects which formed part of Old High German. In the south, the Lombards , who had settled in Northern Italy , maintained their dialect until their conquest by Charlemagne in 774. After this the Germanic-speaking population, who were by then almost certainly bilingual, gradually switched to the Romance language of the native population , so that Langobardic had died out by
4880-444: 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
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#17327656716524960-426: 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 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
5040-459: 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,
5120-506: 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
5200-424: 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
5280-498: The past participle. Initially the past participle retained its original function as an adjective and showed case and gender endings - for intransitive verbs the nominative, for transitive verbs the accusative. For example: After thie thö argangana warun ahtu taga ( Tatian , 7,1) "When eight days had passed", literally "After that then gone-by were eight days" Latin: Et postquam consummati sunt dies octo (Luke 2:21) phīgboum habeta sum giflanzotan (Tatian 102,2) "There
5360-420: The prefaces to his Evangelienbuch , offers comments on and examples of some of the issues which arise in adapting the Latin alphabet for German: " ...sic etiam in multis dictis scriptio est propter litterarum aut congeriem aut incognitam sonoritatem difficilis. " ("...so also, in many expressions, spelling is difficult because of the piling up of letters or their unfamiliar sound.") The careful orthographies of
5440-469: The same as in Middle High German.) The main difference between Old High German and the West Germanic dialects from which it developed is that the former underwent the Second Sound Shift . The result of the sound change has been that the consonantal system of German is different from all other West Germanic languages, including English and Low German . This list has the sound changes that transformed Common West Germanic into Old High German but not
5520-405: The sort on which modern dialect maps are based. For this reason the dialects may be termed "monastery dialects" (German Klosterdialekte ). The main dialects, with their bishoprics and monasteries : In addition, there are two poorly attested dialects: The continued existence of a West Frankish dialect in the Western, Romanized part of Francia is uncertain. Claims that this might have been
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
5680-412: 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
5760-567: 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
5840-468: The transition to Middle High German . Surviving Old High German texts were all composed in monastic scriptoria , so the overwhelming majority of them are religious in nature or, when secular, belong to the Latinate literary culture of Christianity . The earliest instances, which date to the latter half of the 8th century, are glosses —notes added to margins or between lines that provide translation of
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
6000-602: The weakening of unstressed vowels in the endings of nouns and verbs (see above). The early part of the period saw considerable missionary activity, and by 800 the whole of the Frankish Empire had, in principle, been Christianized. All the manuscripts which contain Old High German texts were written in ecclesiastical scriptoria by scribes whose main task was writing in Latin rather than German. Consequently,
6080-540: Was a fig tree that some man had planted", literally "Fig-tree had certain ( or someone) planted" Latin: arborem fici habebat quidam plantatam (Luke 13:6) In time, however, these endings fell out of use and the participle came to be seen no longer as an adjective but as part of the verb, as in Modern German. This development is taken to be arising from a need to render Medieval Latin forms, but parallels in other Germanic languages (particularly Gothic, where
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 ,
6240-697: Was some attempt at conquest and missionary work under the Ottonians . The Alemannic polity was conquered by Clovis I in 496, and in the last twenty years of the 8th century Charlemagne subdued the Saxons, the Frisians, the Bavarians, and the Lombards, bringing all continental Germanic-speaking peoples under Frankish rule. While this led to some degree of Frankish linguistic influence , the language of both
6320-511: Was the neglect or religious zeal of later generations that led to the loss of these records. Thus, it was Charlemagne's weak successor, Louis the Pious , who destroyed his father's collection of epic poetry on account of its pagan content. Rabanus Maurus , a student of Alcuin and later an abbot at Fulda, was an important advocate of the cultivation of German literacy. Among his students were Walafrid Strabo and Otfrid of Weissenburg . Towards
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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