74:
49:
518:
instantaneous maximal flowrate 2 (IMFR2) and IMFR5 metrics were 61 and 85 cubic metres per second (2,200 and 3,000 cu ft/s) respectively. The IMFR10, or flow rate calculated from the 10-year flood, is 100 cubic metres per second (3,500 cu ft/s), the IMFR20 is 120 cubic metres per second (4,200 cu ft/s) and the IMFR50 was 140 cubic metres per second (4,900 cu ft/s). These values are of the order of a fifth of those of the
29:
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510:
81:
56:
559:
487:
The
Vologne exhibits quite marked seasonal variations in flow rate, as is often seen in Eastern France, with winter–spring high water bringing the monthly flow rate to a level between 10.9 and 14.6 cubic metres per second (380 and 520 cu ft/s) from November to April inclusive with a maximum
695:
has been protected since 8 December 1910. Only the part within the commune of
Granges, about 4.5 kilometres (2.8 mi), benefits from protection. This valley is flanked by two steep slopes rising from 250 to 300 metres (820 to 980 ft) that are covered from the base to the summit with ancient
525:
The
Vologne is a very substantial river despite the relative smallness of its basin. The rainfall of the Vosges region which feeds it is also very significant. The runoff curve number in its watershed is 868 millimetres (34.2 in) annually, which is very high, almost three times the ensemble
517:
Flooding of the
Vologne can also be significant. Thus the maximum instantaneous flow rate recorded was 143 cubic metres per second (5,000 cu ft/s) on 9 April 1983, while the maximum daily average flow rate was 108 cubic metres per second (3,800 cu ft/s) the following day. The
522:, and thus comparable when one takes into account the respective extents of their watersheds. It also appears from this that the floods of April 19 discussed above were of the order of 50-year floods, i.e. which might be expected to occur twice per century.
741:
488:
in
February. The low water for July to September brings the average monthly flow rate down to 3.89 cubic metres per second (137 cu ft/s) in August. Nonetheless, these are only averages and there are significant fluctuations over short times.
476:
department situated slightly before its confluence with the
Moselle. The river's watershed at that point is 355 square kilometres (137 sq mi), almost the entire watershed, which is 369 square kilometres (142 sq mi).
538:, a quality rating of 1B, or "bonne" (good) during each of the years in the 10-year period 1997–2006, except in 2002, when the river achieved level 1A, or "très bonne" (very good). In 2006 a slightly excessive level of
632:
The textile industry itself has now almost disappeared, and while this is a cultural, economic and social setback, it has afforded the
Vologne a steady improvement in water quality over recent years. Its high
712:
line and the road occupy the bottom of the valley, whose width, at certain places, is no more than 20 to 25 metres (66 to 82 ft); the slopes are so close to each other that the sun can barely penetrate.
505:
At low water, the 3-year low instantaneous flow rate can drop to 0.99 cubic metres per second (35 cu ft/s) in the case of a dry five-year period, which is low but normal for
Eastern French regions.
526:
average over France, and almost twice the French basin of the
Moselle, 445 millimetres (17.5 in) at Hauconcourt. The specific flow rate reaches 27.4 litres per second per square kilometre of basin.
73:
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of about 80 years. This substantial lifetime gives rise to a very slow regeneration rate for the population, which in turn explains the
821:
48:
708:. The Vologne flows at the foot of the valley, past naturally growing trees and dark rocks which line its route. The river, the
638:
574:
of the
Vologne" were harvested. Their harvest is attested from the 16th century. The pearls, rather small, were prized by the
582:
up until the 19th century, at which time their rarity caused interest to wane. Pearl fishing was regulated and overseen by "
676:
775:
1068:
814:
165:
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Mean monthly flow rate (in m/s) measured at the Cheniménil hydrological station – data calculated over 40 years
293:
937:
602:
473:
321:
679:, was found in the Vologne near Docelles. The case was highly publicised in France and became known as the
1032:
1007:
481:
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In 2006, the Rhine-Meuse water agency assigned the Vologne's water analysed at the level of
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135:
28:
962:
610:
563:
519:
353:
305:
272:
907:
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were observed, but with an oxygen saturation of 79 percent (or 7.9 mg/L) the
464:
The Vologne is a substantial river, as a result of its neighbours in the region of the
385:
484:
of the Vologne at Cheniménil is 9.70 cubic metres per second (343 cu ft/s).
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587:
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in the Vosges department. Places to visit there, aside from the lakes, include the
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34:
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772:"Rhine-Meuse water agency – Water Information system: Qualité des cours d'eau"
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180:
167:
952:
622:
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609:). They measure about 11 by 5 centimetres (4.3 by 2.0 in) and have a
300:, on the northwestern slope of the Hohneck. It flows through the lakes of
598:
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The Vologne near Deycimont, slightly above the confluence with the Barba
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838:
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151:
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Heights and flowrates of the Vologne at Cheniménil – Vigicrues website
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population density won it the right to hold certain rounds of the
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571:
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897:
697:
810:
368:. It flows by Granges-sur-Vologne, receives the Corbeline, the
499:
468:. Its flow rate has been observed for a period of 40 years at
388:
has an area of 369 square kilometres (142 sq mi).
376:) and the Barba at Docelles, then flows into the Moselle at
759:
Banque Hydro – Station A4362030 – The Vologne at Cheniménil
586:" watchers. The name of lordly residence which dominates
667:(category 1 watercourse) over the whole of its length.
644:
The upper Vologne valley is a popular destination for
570:
Until the beginning of the 20th century, the famous "
384:. It is 49.6 kilometres (30.8 mi) long and its
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675:On 16 October 1984, the body of a four-year-old,
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8:
746:"Fiche cours d'eau - La Vologne (A43-0200)"
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815:
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683:. As of 2021 the case remains unsolved.
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508:
344:The source of the Vologne is within the
733:
601:which produce these pearls are called
18:
271:
230:9.70 m/s (343 cu ft/s)
7:
594:, refers to the old pearl industry.
480:The interannual mean flow rate, or
346:Jardin d'altitude du Haut Chitelet
14:
761:(don't tick "Station en service")
665:cours d'eau de première catégorie
660:(Fairies' Bridge) built in 1763.
208:369 km (142 sq mi)
936:
79:
72:
54:
47:
27:
639:World Fly Fishing Championships
80:
55:
159: • coordinates
1:
1064:Rivers of Vosges (department)
621:, certainly, but also to the
113:Physical characteristics
663:The Vologne is classed as a
566:is traversed by the Vologne.
395:
607:Margaritifera margaritifera
328:, finally flowing into the
131: • location
1085:
1054:Tributaries of the Moselle
693:de la Vallée de la Vologne
397:
226: • average
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837:Tributaries of the river
380:, 10 km upstream of
234:
212:
141:
117:
41:
26:
723:List of rivers in France
687:Environmental protection
617:of the species owing to
603:freshwater pearl mussels
348:. It flows through the
200:50 km (31 mi)
652:cascade on an ancient
567:
514:
561:
512:
356:before receiving the
269:French pronunciation:
88:Show map of Grand Est
472:, a locality in the
322:LĂ©panges-sur-Vologne
276:) is a river of the
181:48.11389°N 6.56694°E
1069:Rivers of Grand Est
615:quasi-disappearance
554:History and economy
350:lake of Retournemer
318:Granges-sur-Vologne
239:Basin features
177: /
691:The site known as
568:
515:
421:Stream of Chaufour
63:Show map of France
1041:
1040:
627:textile factories
605:(scientific name
592:Château sur Perle
457:
456:
308:, and passes the
261:
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186:48.11389; 6.56694
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1059:Rivers of France
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783:
774:. Archived from
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750:
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677:Grégory Villemin
671:Grégory Villemin
625:of the river by
550:was sufficient.
466:Vosges Mountains
396:
366:Lac de GĂ©rardmer
314:Xonrupt-Longemer
298:Vosges Mountains
284:. It is a right
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136:Vosges Mountains
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681:Affaire Grégory
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611:life expectancy
564:Lac de Longemer
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354:Lac de Longemer
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273:[vɔlɔɲ]
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33:The Vologne at
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16:River in France
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793:External links
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656:lock, and the
650:Saut des Cuves
641:in July 2002.
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386:drainage basin
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778:on 2007-10-30
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658:Pont des FĂ©es
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530:Water quality
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780:. Retrieved
776:the original
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540:ammonium (NH
533:
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343:
264:
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1003:Ahringsbach
993:Feller Bach
868:Rupt de Mad
799:(in French)
700:, enormous
576:bourgeoisie
548:oxygenation
392:Tributaries
302:Retournemer
244:Progression
184: /
1048:Categories
1008:Kautenbach
782:2011-09-23
729:References
588:Cheniménil
470:Cheniménil
407:Belbriette
404:Balveurche
372:(south of
296:is in the
205:Basin size
1018:Flaumbach
983:Avelsbach
953:Moselotte
923:Brohlbach
623:pollution
482:discharge
460:Hydrology
448:Malenrupt
424:Corbeline
413:Martimpré
340:Geography
286:tributary
256:North Sea
217:Discharge
169:48°6′50″N
35:Beauménil
1013:LĂĽtzbach
858:Terrouin
717:See also
599:molluscs
580:nobility
578:and the
536:Jarménil
431:Bas Prés
378:Jarménil
374:Bruyères
362:spillway
326:Docelles
310:villages
306:Longemer
172:6°34′1″E
98:Location
1033:Ehrbach
1028:Baybach
963:Meurthe
958:Vologne
839:Moselle
710:railway
654:glacial
646:tourism
619:fishing
544:+) ions
520:Meurthe
442:Lizerne
417:Jamagne
358:Jamagne
334:Pouxeux
330:Moselle
290:Moselle
288:of the
265:Vologne
248:Moselle
152:Moselle
103:Country
22:Vologne
968:Seille
918:Endert
908:Lieser
883:Gander
878:Fensch
742:Sandre
590:, the
572:pearls
474:Vosges
382:Épinal
294:source
292:. Its
282:France
278:Vosges
220:
197:Length
125:
122:Source
107:France
998:Dhron
988:Ruwer
893:Sauer
853:Madon
706:scree
702:rocks
698:trees
635:trout
451:Barba
438:Neuné
434:Clous
370:Neuné
252:Rhine
147:Mouth
973:Saar
903:Salm
898:Kyll
888:Syre
873:Orne
863:Esch
597:The
562:The
360:, a
352:and
324:and
304:and
263:The
928:Elz
913:Alf
704:or
364:of
332:in
312:of
1050::
744:.
629:.
336:.
320:,
316:,
254:→
250:→
830:e
823:t
816:v
785:.
748:.
542:4
267:(
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