Search over 40,000 articles from the original, classic Encyclopedia Britannica, 11th Edition.
|
See also:RHONE (Fr. Rhone, See also:Lat. Rhodanus) , one of the most important See also:rivers in See also:Europe, and the See also:chief of those which flow directly into the Mediterranean . It rises at the upper or eastern extremity of the Swiss See also:canton of the See also:Valais, flows between the Bernese See also:Alps (N.) and the Lepontine and Pennine Alps (S.) till it expands into the See also:Lake, of See also:Geneva, winds See also:round the southernmost spurs of the See also:Jura range, receives at See also:Lyons its See also:principal tributary, the See also:Saone, and then turns southward through See also:France till, by many mouths, it enters that See also:part of the Mediterranean which is rightly called the Golfe du See also:Lion (sometimes wrongly the Gulf of Lyons) . Its See also:total length' from source to See also:sea is 5041 M . (of which the Lake of Geneva claims 45 m.), while its total drainage See also:area in 37,798 sq. m., of which 2772 sq. m. are in See also:Switzerland -(405 sq. in. of the Swiss portion being composed of glaciers), and its total fall 5898 ft . Its course (excluding the Lake of Geneva, q.v.) naturally falls into three divisions: (I) from its source to the Lake of Geneva, (2) from Geneva to Lyons, and (3) from Lyons to the Mediterranean . 1 . From its source to the lake the See also:Rhone is a purely Alpine See also:river, flowing through the See also:great See also:trench which it has cut for itself between two of the loftiest Alpine ranges, and which (See also:save a See also:bit at its See also:north-See also:west end) forms the Canton of the Valais . Its length is 1051 m., while its fall is 4679 ft . It issues as a torrent, at the height of 5909 ft., from the great Rhone See also:glacier at the See also:head of the Valais, the See also:recent See also:retreat of this glacier having proved that the river really flows from beneath it, and does not take its rise from the warm springs that are now at some distance from its shrunken snout . It is almost immediately joined on the See also:left by the Mutt torrent, coming from a small glacier to the S.E., and then flows S.W. for a See also:short distance past the well-known Gletsch Hotel (where the roads from the Grimsel and the Furka Passes unite) . But about See also:half a mile from the glacier the river turns S.E. and descends through a See also:wild See also:gorge to the more level valley, bending again S.W. before reaching the first See also:village, Oberwald . It preserves this See also:south-See also:westerly direction till Martigny . The uppermost valley of the Rhone is named Goms (Fr . Conches), its chief village being See also:Munster, while Fiesch, See also:lower down, is well known to most Swiss travellers . As the river rolls on, it is swollen by See also:mountain torrents, descending from the glaciers on either See also:side of its See also:bed—so by the Geren (left), near Oberwald, by the Eginen (left), near Ulrichen, by the Fiesch (right), at Fiesch, by the Binna (left), near Grengiols, by the See also:Massa (right), flowing from the great Aletsch glaciers, above See also:Brieg . At Brieg the Rhone has descended 3678 ft. from its source, has flowed 28 m. in the open, and is already a consider-able stream when joined (left)by the Saltine, descending from the Simplon Pass . Its course below Brieg is less rapid than before and lies through the alluvial deposits which it has brought down in the course of ages . The valley is wide and marshy, the river frequently overflowing its See also:banks, Further mountain torrents (of greater See also:volume than those higher up) fall into the Rhone as it rolls along in a south-westerly direction towards Martigny: the Visp (left), coming from the See also:Zermatt valley, falls in at Visp, at Gampel the Lonza (right), from the Ldtschen valley, at See also:Leuk the Dala (right), from the Gemmi Pass, al . Sierre the Navizen (left), from the Einfisch or Anniviers valley, at See also:Sion, the See also:capital of the Valais, the Borgne (left) from the Val d'Herens; soon the Rhone is joined by the Morge (right), flowing from the Sanetsch Pass, and the boundary in the See also:middle ages between Episcopal Valais to the See also:east and Savo-yard Valais to the west, and at Martigny by the Dranse (left) its chief Alpine tributary, from the Great St See also:Bernard and the Val de Bagnes . At Martigny, about 50 M. from Brieg, the river bends sharply to the N.W., and runs in that direction to the Lake of Geneva . It receives the Salanfe (left), which forms the celebrated See also:waterfall of Pissevache, before reaching the See also:ancient See also:town and See also:abbey of St See also:Maurice (91m.) . Henceforward the right See also:bank is in the canton of See also:Vaud (conquered from See also:Savoy in 1475) and the left bank in that of the Valais (conquered similarly in 1536), for St Maurice marks the end of the See also:historical Valais . Immediately below that town the Rhone rushes through a great natural gateway, a narrow and striking See also:defile (now strongly fortified), which commands the entrance of the Valais . Beyond, the river enters the wide alluvial See also:plain, formerly occupied by the south-eastern See also:arm of the Lake of Geneva, but now marshy and requiring frequent " correction." It receives at Bex the Avancon (right), flowing from the glaciers of the Diablerets range, at Monthey the Vieze (left), from Champery and the Val d'Illiez, and at Aigle the Grande Eau (right), from the valley of Ormonts-dessus . It passes by the See also:hamlet of See also:Port Valais, once on the See also:shore of the lake, before expanding into the Lake of Geneva, between See also:Villeneuve (right) and St Gingolph (left) . During all this portion of its course the Rhone is not navigable, but a railway See also:line runs along it from Brieg in about 72 M. to either Villeneuve or Le Bouveret . 2 . On issuing at Geneva from the lake the See also:waters of the Rhone are very limpid and See also:blue, as it has left all its impurities in the great settling vat of the lake, so that See also:Byron might well speak of the "blue rushing of the arrowy Rhone" (Childe Harold, See also:canto iii. See also:stanza 71) . 'But about half a mile below Geneva this limpidity is disturbed by the pouring in of the turbid torrent of the Arve (left), descending from the glaciers of the Mont See also:Blanc range, the two currents for some distance refusing to mix . The distance from Geneva to Lyons by the tortuous course of the Rhone is about 124 m., the fall being only about 689 ft . The characteristic feature of this portion of the course of the Rhone is the number of narrow See also:gorges or cluses through which it rushes, while it is forced by the See also:southern See also:spur of the Jura to run in a southerly direction, till, after rounding the See also:base of that spur, it can flow freely westwards to Lyons . About 12 M . S. of Geneva the Rhone enters See also:French territory, and henceforth till near Lyons forms first the eastern, then the southern boundary of the French See also:department of the See also:Ain, dividing it from those of Haute See also:Savoie and Savoie (E.) and that of the See also:Isere (S.) . Soon after it becomes French the river rushes furiously through a deep gorge, being imprisoned on the north by the Credo and on the south by the Vuache, while the great fortress of l'Ecluse See also:guards this , entrance into France . The railway pierces the Credo by a See also:tunnel . In the narrowest portion of this gorge, not far from See also:Bellegarde at its lower end, there formerly existed the famous Perte du Rhone (described by See also:Saussure in his Voyages daps See also:les Alpes, See also:chapter xvii.), where for a certain distance the river disappeared in a subterranean channel; but this natural phenomenon has been destroyed, partly by See also:blasting, and partly by the diversion of the See also:water for the use of the factories of Bellegarde .
At Bellegarde the Valserine flows in (right), and then the river resumes its southerly direction, from which the great gorge had deflected it for a while
.
Some way below Bellegarde, between Le Parc and Pyrimont, the
Rhone becomes officially " navigable," though as far as Lyons (1906) 858,907
.
Area, 1104 sq m
.
Rhone is bounded N. by the See also:navigation now consists all but wholly of the floating of the department of Saone-et-See also:Loire, E. by Ain and Isere and S. and See also:flat-bottomed boats, named rigues, laden chiefly with See also: See also:Snow the Jura . It flows past Yenne (left) and beneath the picturesque sometimes lies in the mountains from See also:November to See also:April, fortress (formerly a Carthusian monastery) of See also:Pierre Chatel while at Lyons and in the valleys the mean temperature in See also:winter (right) before it attains the foot of the extreme southern spur of is 36° F. and in summer 70°, the See also:annual mean being 53° . The the Jura, at a height of 696 ft., not far from the village of See also:Cordon, See also:average rainfall is somewhat higher than is See also:general over France and just where the .Guiers flows in (left) from the mountains owing to the amount of the precipitation on the hilly region . of the Grande See also:Chartreuse . This is nearly the last of the cluses See also:Good agricultural See also:land is found in the valleys of the Saone through which the river has to make its way . The very last and Rhone, but for the most part the See also:soil is stony and only is at the See also:Pont du Saut or Sault, a little S. of Lagnieu . The river moderately fertile . See also:Wheat, oats, See also:rye and potatoes are ex-now widens, but the neighbouring See also:country is much exposed to tensively cultivated, but their importance is less than that of inundations . It receives (right) its most important tributary the See also:vine, the hills of the Beaujolais on the right bank of the in this part of its course, the Ain, which descends from the Saone producing excellent wines . See also:Fruit trees, such as peaches, French slope of the Jura and is navigable for about 6o m. above apricots, walnuts and chestnuts, grow well, but the See also:wood in its junction with the Rhone . Farther down the Rhone meanders general is little more than copse and brushwood . Good for a See also:time with shifting channels in a bed about 2 M. broad, pasture is found in the valleys of the Azergues and its affluents. but it gathers into a single stream before its junction with the Mines of See also:iron-See also:pyrites and See also:coal and quarries of freestone are Saone, just below Lyons . The Saone (q.v.), which has received worked .. The See also:production of See also:silk fabrics, the chief See also:branch of (left) the See also:Doubs, is the real continuation of the Rhone, both manufacture, that of chemicals and machinery, together with from a See also:geographical and a commercial point of view, and it is most of the other See also:industries of the department, are concentrated by means of canals branching off from the course of the Saone in Lyons (q.v.) and its vicinity . Tarare is a centre for the that the Rhone communicates with the basins of the Loire, manufacture of See also:muslin and See also:embroidery . Oullins has large the See also:Seine, the See also:Rhine and the Moselle . In fact, up to Lyons, railway workshops belonging to the See also:Paris-See also:Lyon-Mediterranee the Rhone (save when it expands into the Lake of Geneva) is railway, and there are important See also:glass See also:works at See also:Givors . See also:Cotton-a huge and very unruly mountain torrent rather than a great See also:spinning and See also:weaving are carried on in several localities . The See also:European river. products of its manufactures, together with See also:wine and See also:brandy, 3 . Below Lyons, however, the Rhone becomes one of the form the bulk of the exports of the department; its imports great historical rivers of France . It was up its valley that comprise chiefly the raw material for its industries . It is first See also:Greek, 'then Latin .See also:civilization penetrated from the Medi- served by the Paris-Lyon railway . The Rhone and the Saone terranean to Lyons, as well as in the loth See also:century the Saracen and in the extreme south the canal of Givors are its navigable bandits from their See also:settlement at La Garde Freinet, near the waterways . Lyons the capital is the seat of an See also:archbishop See also:coast of See also:Provence . Then, too, from Lyons downwards, the and of a See also:court of See also:appeal and centre of an educational See also:division Rhone serves as a great See also:medium of See also:commerce by which central (academie) . The department is divided amongst the districts France sends its products to the sea . Its length from Lyons of the VII., VIII., XIL, XIII. and XIV. See also:army See also:corps . There to the sea is some 230 m., though its fall is but 530 ft . But are two arrondissements (Lyons and Villefranche) subdivided during this half of its course it can boast of having on its left into 29 cantons and 269 communes . The principal places bank (the right bank is very poor in this respect) such historical besides Lyons are Givors, Tarare and Villefranche, which cities as See also:Vienne, See also:Valence, See also:Avignon, See also:Tarascon and See also:Arles, while receive See also:separate treatment . it receives (left) the Isere, the See also:Drome and the See also:Durance rivers, RHONGEBIRGE, or See also:DIE RHoN, a mountain-See also:chain of central all formed by the See also:union of many streams, and bringing down See also:Germany, See also:running in a north-westerly direction from the the waters that flow from the lofty snowy See also:Dauphine Alps . Bavarian See also:province of Lower See also:Franconia to the Prussian province The See also:Ardeche is the only considerable affluent from the right. of See also:Hesse-See also:Nassau and the See also:grand duchy of See also:Saxe-See also:Weimar, and Near Arles, about 25 M. from the sea, and by rail 1754 M. from divided by the Werra from the Thuringian See also:Forest on the N . Lyons, the river breaks up into its two See also:main branches, the The other sides are bounded by the See also:Fulda on the W. and the Grand Rhone running S.E. and the See also:Petit Rhone S.W.; they Sinn and Frankish Saab on the E. and S . Its length is 50 m., enclose between them the huge See also:delta of the See also:Camargue, which breadth 5-7 m., and its mean elevation 1900 ft . This See also:district is cultivated on the banks of the river only, but elsewhere is is divided into three groups—the southern, the high (Hohe) simply a great alluvial plain, deposited in the course of ages and the nearer (Vordere) Rhon . Of these the southern, a con-by the river, and now composed of scanty pasturages and of tinuation of the See also:Spessart, largely consists of flat conical masses great See also:salt marshes . Between Lyons and the sea, the Rhone and reaches its highest point in the Heiliger Kreuzberg (2966 ft.). divides four departments on its right bank (Rhone, Loire, The Hohe Rhon, beginning immediately to the north-west of Ardeche and See also:Gard) from as many on its left bank (Isere, the latter mountain, is a high See also:plateau of red See also:sandstone, covered See also:Dame, See also:Vaucluse and Bouches du Rhone). with See also:fens and See also:basalt peaks . It is a wild, dreary, inclement Consult in general Ch . Lentheric, Le Rhone—histoire d'un ,fleuve, See also:tract of country, covered with snow for six months in the See also:year 2 vols . (Paris, 1892) . (W . A . B . C.) and visited by frequent fogs and storms . |
|
|
[back] RHONE |
[next] RHOXOLANI |
There are no comments yet for this article.
Do not copy, download, transfer, or otherwise replicate the site content in whole or in part.
Links to articles and home page are encouraged.