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52-575: Le Châtelet-sur-Meuse ( French pronunciation: [lə ʃatlɛ syʁ møz] , literally Le Châtelet on Meuse ) is a commune in the Haute-Marne department in north-eastern France . It contains the source of the River Meuse , which is very close to the commune's village of Pouilly-en-Bassigny. [REDACTED] This geography Haute-Marne article is a stub . You can help Misplaced Pages by expanding it . Meuse From 1301,

104-667: A common history of pre-Proto-Germanic speakers throughout the Nordic Bronze Age . The Proto-Germanic language developed in southern Scandinavia (Denmark, south Sweden and southern Norway) and the northern-most part of Germany in Schleswig Holstein and northern Lower Saxony, the Urheimat (original home) of the Germanic tribes. It is possible that Indo-European speakers first arrived in southern Scandinavia with

156-432: A dialect of Proto-Indo-European that had lost its laryngeals and had five long and six short vowels as well as one or two overlong vowels. The consonant system was still that of PIE minus palatovelars and laryngeals, but the loss of syllabic resonants already made the language markedly different from PIE proper. Mutual intelligibility might have still existed with other descendants of PIE, but it would have been strained, and

208-475: A larger scope of linguistic developments, spanning the Nordic Bronze Age and Pre-Roman Iron Age in Northern Europe (second to first millennia BC) to include "Pre-Germanic" (PreGmc), "Early Proto-Germanic" (EPGmc) and "Late Proto-Germanic" (LPGmc). While Proto-Germanic refers only to the reconstruction of the most recent common ancestor of Germanic languages, the Germanic parent language refers to

260-555: A late stage. The early stage includes the stress fixation and resulting "spontaneous vowel-shifts" while the late stage is defined by ten complex rules governing changes of both vowels and consonants. By 250 BC Proto-Germanic had branched into five groups of Germanic: two each in the West and the North and one in the East. The following changes are known or presumed to have occurred in

312-807: Is largely a matter of convention. The first coherent text recorded in a Germanic language is the Gothic Bible , written in the later fourth century in the East Germanic variety of the Thervingi Gothic Christians , who had escaped persecution by moving from Scythia to Moesia in 348. Early West Germanic text is available from the fifth century, beginning with the Frankish Bergakker runic inscription . The evolution of Proto-Germanic from its ancestral forms, beginning with its ancestor Proto-Indo-European , began with

364-413: Is termed Pre-Proto-Germanic . Whether it is to be included under a wider meaning of Proto-Germanic is a matter of usage. Winfred P. Lehmann regarded Jacob Grimm 's "First Germanic Sound Shift", or Grimm's law, and Verner's law , (which pertained mainly to consonants and were considered for many decades to have generated Proto-Germanic) as pre-Proto-Germanic and held that the "upper boundary" (that is,

416-695: 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 branches during the fifth century BC to fifth century AD: West Germanic , East Germanic and North Germanic . The latter of these remained in contact with the others over a considerable time, especially with the Ingvaeonic languages (including English ), which arose from West Germanic dialects, and had remained in contact with

468-564: Is the question of what specific tree, in the tree model of language evolution, best explains the paths of descent of all the members of a language family from a common language, or proto-language (at the root of the tree) to the attested languages (at the leaves of the tree). The Germanic languages form a tree with Proto-Germanic at its root that is a branch of the Indo-European tree, which in turn has Proto-Indo-European at its root. Borrowing of lexical items from contact languages makes

520-548: Is typical not of Germanic but Celtic languages. Another is * walhaz 'foreigner; Celt' from the Celtic tribal name Volcae with k → h and o → a . Other likely Celtic loans include * ambahtaz 'servant', * brunjǭ 'mailshirt', * gīslaz 'hostage', * īsarną 'iron', * lēkijaz 'healer', * laudą 'lead', * Rīnaz 'Rhine', and * tūnaz, tūną 'fortified enclosure'. These loans would likely have been borrowed during

572-677: The Corded Ware culture in the mid-3rd millennium BC, developing into the Nordic Bronze Age cultures by the early second millennium BC. According to Mallory, Germanicists "generally agree" that the Urheimat ('original homeland') of the Proto-Germanic language, the ancestral idiom of all attested Germanic dialects, was primarily situated in an area corresponding to the extent of the Jastorf culture . Early Germanic expansion in

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624-503: The Funnelbeaker culture , but the sound change in the Germanic languages known as Grimm's law points to a non-substratic development away from other branches of Indo-European. Proto-Germanic itself was likely spoken after c. 500 BC, and Proto-Norse , from the second century AD and later, is still quite close to reconstructed Proto-Germanic, but other common innovations separating Germanic from Proto-Indo-European suggest

676-794: The Langres plateau in France from where it flows northwards past Sedan (the head of navigation ) and Charleville-Mézières into Belgium. At Namur it is joined by the Sambre . Beyond Namur the Meuse winds eastwards and passes Liège before turning north. The river then forms part of the Belgian-Dutch border, except that at Maastricht the border lies further to the west. In the Netherlands it continues northwards through Venlo closely along

728-637: The Norse . A defining feature of Proto-Germanic is the completion of the process described by Grimm's law , a set of sound changes that occurred between its status as a dialect of Proto-Indo-European and its gradual divergence into a separate language. The end of the Common Germanic period is reached with the beginning of the Migration Period in the fourth century AD. The alternative term " Germanic parent language " may be used to include

780-742: The Oude Maasje . In the late 19th century and early 20th century the connection between the Maas and Rhine was closed off and the Maas was given a new, artificial mouth – the Bergse Maas . The resulting separation of the rivers Rhine and Maas reduced the risk of flooding and was considered to be the greatest achievement in Dutch hydraulic engineering before the completion of the Zuiderzee Works and Delta Works . The former main branch was, after

832-681: The Pre-Roman Iron Age (fifth to first centuries BC) placed Proto-Germanic speakers in contact with the Continental Celtic La Tène horizon . A number of Celtic loanwords in Proto-Germanic have been identified. By the first century AD, Germanic expansion reached the Danube and the Upper Rhine in the south and the Germanic peoples first entered the historical record . At about the same time, extending east of

884-621: The Vistula ( Oksywie culture , Przeworsk culture ), Germanic speakers came into contact with early Slavic cultures, as reflected in early Germanic loans in Proto-Slavic . By the third century, Late Proto-Germanic speakers had expanded over significant distance, from the Rhine to the Dniepr spanning about 1,200 km (700 mi). The period marks the breakup of Late Proto-Germanic and

936-604: The battle , which saw the men from Liège defeated, John ordered the drowning in the Meuse of burghers and noblemen in Liège whose loyalties he suspected. The border remained relatively stable until the annexation of the Three Bishoprics Metz, Toul and Verdun by King Henry II in 1552 and the occupation of the Duchy of Lorraine by the forces of King Louis XIII in 1633. Its lower Belgian ( Walloon ) portion, part of

988-455: The sillon industriel , was the first fully industrialized area in continental Europe. The Afgedamde Maas was created in the late Middle Ages, when a major flood made a connection between the Maas and the Merwede at the town of Woudrichem . From that moment on, the current Afgedamde Maas was the main branch of the lower Meuse. The former main branch eventually silted up and is today called

1040-484: The "lower boundary" was the dropping of final -a or -e in unstressed syllables; for example, post-PIE * wóyd-e > Gothic wait , 'knows'. Elmer H. Antonsen agreed with Lehmann about the upper boundary but later found runic evidence that the -a was not dropped: ékwakraz … wraita , 'I, Wakraz, … wrote (this)'. He says: "We must therefore search for a new lower boundary for Proto-Germanic." Antonsen's own scheme divides Proto-Germanic into an early stage and

1092-556: The 2nd century CE, as well as the non-runic Negau helmet inscription, dated to the 2nd century BCE), and in Roman Empire -era transcriptions of individual words (notably in Tacitus ' Germania , c. AD 90 ). Proto-Germanic developed out of pre-Proto-Germanic during the Pre-Roman Iron Age of Northern Europe. According to the Germanic substrate hypothesis , it may have been influenced by non-Indo-European cultures, such as

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1144-429: The Germanic subfamily exhibited a less treelike behaviour, as some of its characteristics were acquired from neighbours early in its evolution rather than from its direct ancestors. The internal diversification of West Germanic developed in an especially non-treelike manner. Proto-Germanic is generally agreed to have begun about 500 BC. Its hypothetical ancestor between the end of Proto-Indo-European and 500 BC

1196-644: The Meuse basin was one of the many regions in Europe to experience catastrophic flooding during the 2021 European floods . The name Meuse is derived from the French name of the river, derived from its Latin name, Mosa , which ultimately derives from the Celtic or Proto-Celtic name * Mosā . This probably derives from the same root as English " maze ", referring to the river's twists and turns. The Dutch name Maas descends from Middle Dutch Mase , which comes from

1248-606: The Meuse but pumps running water into the Meuse). Most of the basin area (approximately 36,000 km ) is in Wallonia (12,000 km ), followed by France (9,000 km ), the Netherlands (8,000 km ), Germany (2,000 km ), Flanders (2,000 km ) and Luxembourg (a few km ). An International Commission on the Meuse has the responsibility of the implementation of the treaty. The costs of this Commission are met by all these countries, in proportion of their own territory in

1300-440: The Meuse has been relatively stable over the last few thousand years. One recent study estimates that average flow has increased by about 10% since 2000 BC. The hydrological distribution of the Meuse changed during the later Middle Ages, when a major flood forced it to shift its main course northwards towards the river Merwede . From then on several stretches of the original Merwede were renamed "Maas" (i.e. Meuse) and served as

1352-418: The Meuse is bypassed by the 36 km (22.4 mi) Juliana Canal . South of Namur, further upstream, the river can only carry more modest vessels, although a barge as long as 100 m (328 ft). can still reach the French border town of Givet. From Givet, the river is canalized over a distance of 272 kilometres (169 mi). The canalized Meuse used to be called the "Canal de l'Est — Branche Nord" but

1404-578: The Rhine distributaries. The resulting separation of the rivers Rhine and Meuse is considered to be the greatest achievement in Dutch hydraulic engineering before the completion of the Zuiderzee Works and Delta Works . In 1970 the Haringvlietdam has been finished. Since then the reunited Rhine and Meuse waters have reached the North Sea either at this site or, during times of lower discharges of

1456-412: The Rhine, at Hook of Holland . A 2008 study notes that the difference between summer and winter flow volumes has increased significantly in the last 100–200 years. It points out that the frequency of serious floods ( i.e. flows > 1000% of normal) has increased markedly. They predict that winter flooding of the Meuse may become a recurring problem in the coming decades. The Meuse flows through

1508-649: The Waal, the main stem of the Rhine at Woudrichem , and then flows under the name of Boven Merwede to Hardinxveld-Giessendam , where it splits into Nieuwe Merwede and Beneden Merwede . Near Lage Zwaluwe , the Nieuwe Merwede joins the Amer, forming the Hollands Diep , which splits into Grevelingen and Haringvliet , before finally flowing into the North Sea. The Meuse is crossed by railway bridges between

1560-599: The basin of the Meuse: Netherlands 30%, Wallonia 30%, France 15%, Germany 14.5%, Flanders 5%, Brussels 4.5%, Kingdom of Belgium 0.5%, and Luxembourg 0.5%. The map of the basin area of Meuse was joined to the text of the treaty. As for culture, as a major communication route the River Meuse is the origin of Mosan art , principally (Wallonia and France). The first landscape painted in the Renaissance

1612-489: The beginning of the (historiographically recorded) Germanic migrations . The earliest available complete sentences in a Germanic language are variably dated to the 2nd century AD, around 300 AD or the first century AD in runic inscriptions (such as the Tune Runestone ). The language of these sentences is known as Proto-Norse , although the delineation of Late Common Germanic from Proto-Norse at about that time

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1664-613: The border to Germany, then turns towards the west, where it runs parallel to the Waal and forms part of the extensive Rhine–Meuse–Scheldt delta , together with the Scheldt to its south and the Rhine to the north. The river has been divided near Heusden into the Afgedamde Maas on the right and the Bergse Maas on the left. The Bergse Maas continues under the name of Amer , which is part of De Biesbosch . The Afgedamde Maas joins

1716-704: The dam at its southern inlet was completed in 1904, renamed Afgedamde Maas and no longer receives water from the Maas. The Meuse and its crossings were a key objective of the Battle of France , the Battle of Sedan and also for the last major German WWII counter-offensive on the Western Front , the Battle of the Bulge in December 1944 and January 1945. The Meuse is represented in the documentary The River People released in 2012 by Xavier Istasse. In July 2021,

1768-498: The dates of borrowings and sound laws are not precisely known, it is not possible to use loans to establish absolute or calendar chronology. Most loans from Celtic appear to have been made before or during the Germanic Sound Shift . For instance, one specimen * rīks 'ruler' was borrowed from Celtic * rīxs 'king' (stem * rīg- ), with g → k . It is clearly not native because PIE * ē → ī

1820-414: The development of a separate common way of speech among some geographically nearby speakers of a prior language and ended with the dispersion of the proto-language speakers into distinct populations with mostly independent speech habits. Between the two points, many sound changes occurred. Phylogeny as applied to historical linguistics involves the evolutionary descent of languages. The phylogeny problem

1872-432: The earlier boundary) was the fixing of the accent, or stress, on the root syllable of a word, typically on the first syllable. Proto-Indo-European had featured a moveable pitch-accent consisting of "an alternation of high and low tones" as well as stress of position determined by a set of rules based on the lengths of a word's syllables. The fixation of the stress led to sound changes in unstressed syllables. For Lehmann,

1924-480: The entire journey that the dialect of Proto-Indo-European that would become Proto-Germanic underwent through the millennia. The Proto-Germanic language is not directly attested by any complete surviving texts; it has been reconstructed using the comparative method . However, there is fragmentary direct attestation of (late) Proto-Germanic in early runic inscriptions (specifically the Vimose inscriptions , dated to

1976-496: The erosion of unstressed syllables, which would continue in its descendants. The final stage of the language included the remaining development until the breakup into dialects and, most notably, featured the development of nasal vowels and the start of umlaut , another characteristic Germanic feature. Loans into Proto-Germanic from other (known) languages or from Proto-Germanic into other languages can be dated relative to each other by which Germanic sound laws have acted on them. Since

2028-1534: The following departments of France , provinces of Belgium , provinces of the Netherlands and towns: Main cities and tributaries will be in bold . France Grand Est Region Haute-Marne Department [REDACTED] Le Châtelet-sur-Meuse [REDACTED] Premier pont de la Meuse [REDACTED] Pont de Malroy [REDACTED] Pont du Pâtis des Vannees [REDACTED] Ruisseau de Pré Chatenay [REDACTED] Pont de Meuse (D429 Val-de-Meuse - Dombrot-le-Sec ) [REDACTED] Ruisseau d'Avrecourt [REDACTED] Railway bridge Culmont-Chalindrey - Toul line [REDACTED] Ru d'Ouette [REDACTED] Ru des Fossés [REDACTED] Ruisseau de Bocheret [REDACTED] Provenchères-sur-Meuse [REDACTED] Pont de Val-de-Meuse (D189) [REDACTED] Ruisseau des Aimeguenons [REDACTED] Pont de l'A31 ( A31 Nancy - Dijon ) [REDACTED] Ruisseau de Joncourt [REDACTED] Pont de D132 [REDACTED] Ruisseau de l'Étange Proto-Germanic Pontic Steppe Caucasus East Asia Eastern Europe Northern Europe Pontic Steppe Northern/Eastern Steppe Europe South Asia Steppe Europe Caucasus India Indo-Aryans Iranians East Asia Europe East Asia Europe Indo-Aryan Iranian Indo-Aryan Iranian Others European Proto-Germanic (abbreviated PGmc ; also called Common Germanic )

2080-586: The following stations (on the left and right banks respectively): There are also numerous road bridges and around 32 ferry crossings. The Meuse is navigable over a substantial part of its total length: In the Netherlands and Belgium, the river is part of the major inland navigation infrastructure, connecting the Rotterdam-Amsterdam-Antwerp port areas to the industrial areas upstream: 's-Hertogenbosch, Venlo, Maastricht, Liège, Namur. Between Maastricht and Maasbracht , an unnavigable section of

2132-545: The history of Proto-Germanic in the wider sense from the end of Proto-Indo-European up to the point that Proto-Germanic began to break into mutually unintelligible dialects. The changes are listed roughly in chronological order, with changes that operate on the outcome of earlier ones appearing later in the list. The stages distinguished and the changes associated with each stage rely heavily on Ringe 2006 , Chapter 3, "The development of Proto-Germanic". Ringe in turn summarizes standard concepts and terminology. This stage began with

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2184-413: The period marked the definitive break of Germanic from the other Indo-European languages and the beginning of Germanic proper, containing most of the sound changes that are now held to define this branch distinctively. This stage contained various consonant and vowel shifts, the loss of the contrastive accent inherited from PIE for a uniform accent on the first syllable of the word root, and the beginnings of

2236-505: The presumed but unattested Old Dutch form * Masa , from Proto-Germanic * Masō . Modern Dutch and German Maas and Limburgish Maos preserve this Germanic form. Despite the similarity, the Germanic name is not derived from the Celtic name, judging from the change from earlier o into a , which is characteristic of the Germanic languages. The Meuse rises in Pouilly-en-Bassigny, commune of Le Châtelet-sur-Meuse on

2288-596: The primary outflow of that river. Those branches are currently known as the Nieuwe Maas and Oude Maas. However during another series of severe floods the Meuse found an additional path towards the sea, resulting in the creation of the Biesbosch wetlands and Hollands Diep estuaries. Thereafter the Meuse split near Heusden into two main distributaries, one flowing north to join the Merwede and one flowing direct to

2340-552: The reduction of the resulting unstressed syllables. By this stage, Germanic had emerged as a distinctive branch and had undergone many of the sound changes that would make its later descendants recognisable as Germanic languages. It had shifted its consonant inventory from a system that was rich in plosives to one containing primarily fricatives, had lost the PIE mobile pitch accent for a predictable stress accent, and had merged two of its vowels. The stress accent had already begun to cause

2392-539: The relative position of the Germanic branch within Indo-European less clear than the positions of the other branches of Indo-European. In the course of the development of historical linguistics, various solutions have been proposed, none certain and all debatable. In the evolutionary history of a language family, philologists consider a genetic "tree model" appropriate only if communities do not remain in effective contact as their languages diverge. Early Indo-European had limited contact between distinct lineages, and, uniquely,

2444-508: The river Meuse. The first fossils of it were discovered outside Maastricht in 1780. An international agreement was signed in 2002 in Ghent , Belgium, about the management of the river amongst France, Germany, Luxembourg , the Netherlands, and Belgium. Also participating in the agreement were the Belgian regional governments of Flanders , Wallonia , and Brussels (which is not in the basin of

2496-413: The sea. The branch of the Meuse leading direct to the sea eventually silted up (and now forms the Oude Maasje stream), but in 1904 the canalised Bergse Maas was dug to take over the functions of the silted-up branch. At the same time the branch leading to the Merwede was dammed at Heusden (and has since been known as the Afgedamde Maas ) so that little water from the Meuse entered the old Maas courses or

2548-511: The separation of a distinct speech, perhaps while it was still forming part of the Proto-Indo-European dialect continuum. It contained many innovations that were shared with other Indo-European branches to various degrees, probably through areal contacts, and mutual intelligibility with other dialects would have remained for some time. It was nevertheless on its own path, whether dialect or language. This stage began its evolution as

2600-640: The upper Meuse roughly marked the western border of the Holy Roman Empire with the Kingdom of France , after Count Henry III of Bar had to receive the western part of the County of Bar ( Barrois mouvant ) as a French fief from the hands of King Philip IV . In 1408, a Burgundian army led by John the Fearless went to the aid of John III against the citizens of Liège, who were in open revolt. After

2652-513: Was recently rebaptized into "Canal de la Meuse". The waterway can be used by the smallest barges that are still in use commercially almost 40 m (131 ft) long and just over 5 metres (16 ft) wide. Just upstream of the town of Commercy, the Canal de la Meuse connects with the Marne–Rhine Canal by means of a short diversion canal. The Cretaceous sea reptile Mosasaur is named after

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2704-415: Was the landscape of Meuse by Joachim Patinir . He was likely the uncle of Henri Blès , who is sometimes defined as a Mosan landscape painter active during the second third of the 16th century (i.e. second generation of landscape painters). The main tributaries of the Meuse are listed below in downstream-upstream order, with the town where the tributary meets the river: The mean annual discharge rate of

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