Moselotte

{{Infobox river

| name = Moselotte

| image = Cornimont Moselotte 20070703 France Vosges Misson Didier.JPG

| image_caption = The Moselotte flowing through Cornimont

| pushpin_map = France#France Grand Est

| source1_location =

| mouth = Moselle

| mouth_coordinates = {{coord|48.0137|6.6147|display=it|region:FR_type:river}}

| progression = {{RMoselle}}

| subdivision_type1 = Country

| subdivision_name1 = France

| length = {{convert|47.3|km|mi|abbr=on}}

| source1_elevation =

| discharge1_avg = {{convert|13.7|m3/s|cuft/s|abbr=on}}

| basin_size = {{convert|356|km2|mi2|abbr=on}}

}}

File:Crosery 3.jpg

The Moselotte ({{IPA|fr|mozlɔt|-|LL-Q150 (fra)-Poslovitch-Moselotte.wav}}) is a river in Lorraine, in the French department of Vosges. It is a direct right tributary of the Moselle, and thus a sub-tributary of the Rhine.

Geography

The Moselotte rises in the massif des Vosges at the fontaine de la Duchesse, near the summit of Hohneck. It flows into the Moselle at Remiremont. Its length is {{convert|47.3|km|mi}},{{sandre|id=A41-0200|nom=La Moselotte}} while its watershed is {{convert|356|km2|mi2}}.

= Communes traversed by the Moselotte =

The Moselotte flows through, from upstream to downstream, the communes of La Bresse, Cornimont, Saulxures, Thiéfosse, Vagney, Saint-Amé, Le Syndicat, Dommartin-lès-Remiremont and Saint-Étienne-lès-Remiremont opposite the town of Remiremont.

= Main tributaries =

The Moselotte is fed by the following tributaries:

valign="top"

|

  • Blanchemer (flows through lac de Blanchemer)
  • Régit
  • Machey
  • Goutte de la Vierge
  • Goutte du Pont d'Air
  • Goutte du Pré Guéry
  • Goutte de Séchemer
  • Goutte du lac des Corbeaux
  • Goutte des Betches
  • Goutte des Ecorces
  • Chajoux (from lac de Lispach)
  • Grande Goutte

|

  • Goutte de la Louvière
  • Goutte du Brabant
  • Goutte du Reucy
  • Goutte du Raindé
  • Goutte du Couchetat
  • Goutte de Parfongoutte
  • Goutte du Droit
  • Xoulces
  • Ventron
  • Géhant
  • Morbieux
  • Rupt de Bâmont

|

  • Amias
  • Grettery
  • Envers des Graviers
  • Envers de Thiéfosse
  • Droit de Thiéfosse
  • Rupt
  • Solem
  • Demixard
  • Pennecières
  • Bouchot
  • Lémont
  • Cleurie.

= Lakes =

The Moselotte watershed includes numerous natural lakes which are often enhanced by a small barrage, including lac de Blanchemer, lac de Lispach and lac des Corbeaux.

The presence of a high barrage at the foot of Kastelberg since 1983 has resulted in the appearance of the lac de la Lande. It collects water from several sources via conduits, and supplies the La Bresse commune with its energy.

At the entry downstream of Saulxures, a lake of {{convert|9.6|ha|acre}} was set up in 1998 under the name lac de la Moselotte which hosts a leisure center.

= Hydrology – at Vagney station =

Like the majority of Vosges rivers, the Moselotte is very substantial. Its flow rate has been observed during a period of 40 years Vagney at a place called Zainvilliers, which is upstream of the Moselotte's confluence with the Moselle.[http://www.hydro.eaufrance.fr/selection.php?consulte=rechercher Banque Hydro – Station A4140202 – La Moselotte à Vagney (option Synthèse)] (don't tick "Station en service") The river's watershed at this point is {{convert|187|km2|mi2}} or 53 percent of its entire watershed, corresponding to the upper half of its course.

The average interannual flow rate, or discharge at Vagney is {{convert|8.54|m3/s|cuft/s}}.

The Moselotte exhibits quite marked seasonal fluctuations, with a winter-spring period of high water whose monthly average flow rate is between {{convert|10.8|and|13.2|m3/s|cuft/s}} from November to April inclusive, with a maximum in December. From the beginning of May, the flow rate falls off rapidly, reaching {{convert|3.06|m3/s|cuft/s}} in August, which is not very severe for a body of water of this size. However year by year fluctuation can be more significant, as can those in the short term.

{{center|

Average monthly flow rate of the Moselotte (m3/s) measured at Vagney hydrological station
Data taken over a 40-year period

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PlotArea = left:40 bottom:40 top:20 right:20

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Period = from:0 till:16

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bar:Jan text:Jan

bar:Fév text:Feb

bar:Mar text:March

bar:Avr text:April

bar:Mai text:May

bar:Jun text:June

bar:Jul text:July

bar:Aoû text:August

bar:Sep text:Sept.

bar:Oct text:Oct.

bar:Nov text:Nov.

bar:Déc text:Déc.

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bar:Jan from:0 till: 12.80

bar:Fév from:0 till: 12.10

bar:Mar from:0 till: 12.00

bar:Avr from:0 till: 10.80

bar:Mai from:0 till: 7.250

bar:Jun from:0 till: 4.940

bar:Jul from:0 till: 3.700

bar:Aoû from:0 till: 3.060

bar:Sep from:0 till: 4.040

bar:Oct from:0 till: 7.830

bar:Nov from:0 till: 11.10

bar:Déc from:0 till: 13.20

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bar:Jan at: 12.80 fontsize:S text: 12,80 shift:(-10,5)

bar:Fév at: 12.10 fontsize:S text: 12,10 shift:(-10,5)

bar:Mar at: 12.00 fontsize:S text: 12,00 shift:(-10,5)

bar:Avr at: 10.80 fontsize:S text: 10,80 shift:(-10,5)

bar:Mai at: 7.250 fontsize:S text: 7,25 shift:(-10,5)

bar:Jun at: 4.940 fontsize:S text: 4,94 shift:(-10,5)

bar:Jul at: 3.700 fontsize:S text: 3,70 shift:(-10,5)

bar:Aoû at: 3.060 fontsize:S text: 3,06 shift:(-10,5)

bar:Sep at: 4.040 fontsize:S text: 4,04 shift:(-10,5)

bar:Oct at: 7.830 fontsize:S text: 7,83 shift:(-10,5)

bar:Nov at: 11.10 fontsize:S text: 11,10 shift:(-10,5)

bar:Déc at: 13.20 fontsize:S text: 13,20 shift:(-10,5)

}}

At low water, the 3-year low instantaneous flow rate can drop to {{convert|0.37|m3/s|cuft/s}} in the case of a dry five-year period, or about {{convert|370|L/s|USgal/s}}, which is quite severe, but typical of rivers in the Moselle basin.

Floods can also be significant particularly bearing in mind the smallness of the watershed, only {{convert|187|km2|mi2}}. The maximum instantaneous flow rates over a 2-year and 5-year period (MIFR2 and MIFR5) measure {{convert|97|and|110|m3/s|cuft/s}} respectively. The MIFR10 is {{convert|120|m3/s|cuft/s}}, the MIFR20 is {{convert|130|m3/s|cuft/s}}, while the MIFR50 rises to {{convert|150|m3/s|cuft/s}}.

The maximum instantaneous flow rate recorded at Vagney was {{convert|121|m3/s|cuft/s}} on 15 February 1990, while the maximum daily average flow rate was {{convert|108|m3/s|cuft/s}} on the same day. Comparing these values to the MIFR measurements for the river suggests that the flood on that day was approximately a 10-year event and thus likely to recur frequently.

Overall the Moselotte is an extremely abundant river in its upper course. The runoff curve number in this 53 percent of its watershed is {{convert|1445|mm|in}} annually, which is extremely high for the northern part of France, and more than four times higher than the French national average. It is also three times higher than the average over the French basin of the Moselle. The specific flow rate attaches to these facts the portentous figure of 45.7 litres per second per square kilometre of watershed.

= Hydrology – at the confluence with the Moselle =

The interannual flow rate/discharge of the Moselotte at its confluence with the Moselle is {{convert|13.7|m3/s|cuft/s}}, for a watershed of {{convert|356|km2|mi2}}.{{cite web |url= http://www2.lorraine.ecologie.gouv.fr/Eau_quantite/cataloguedebits/debitsobserves/moselleamont/moselotte.pdf |title= Characteristic flow rates of the Moselotte |access-date= 2011-09-24 |archive-url= https://web.archive.org/web/20061121213125/http://www.lorraine.ecologie.gouv.fr/Eau_quantite/cataloguedebits/debitsobserves/moselleamont/moselotte.pdf |archive-date= 2006-11-21 |url-status= dead }} The runoff curve number in its watershed is {{convert|1214|mm|in}}, which is very high indeed, not merely much higher than the average for France (by more than a factor of three) with all basins included, but also much higher than the average for the French Moselle basin. In fact, the runoff curve number at Hauconcourt, located slightly downstream of the town of Metz, near where it leaves French territory, rises to {{convert|445|mm|in}}.[http://www.hydro.eaufrance.fr/selection.php Banque Hydro – Station A7930610 – La Moselle à Hauconcourt] (Do not tick the box for "Station en service") The specific flow rate of the Moselotte rises to 38.5 litres per second per square kilometre of watershed. This, along with the Breuchin (a tributary of the Lanterne and sub-tributary of the Saône which flows elsewhere in the same region) constitutes a record for the north third of France.

The Moselotte is clearly more abundant than the Moselle at their confluence, {{convert|13.7|m3/s|cuft/s}} against {{convert|9.3|m3/s|cuft/s}}.{{cite web |url= http://www2.lorraine.ecologie.gouv.fr/Eau_quantite/cataloguedebits/debitsobserves/moselleamont/moselle.pdf |title= Characteristic flow rates of the Moselle upstream |access-date= 2011-09-24 |archive-url= https://web.archive.org/web/20061121182729/http://www.lorraine.ecologie.gouv.fr/Eau_quantite/cataloguedebits/debitsobserves/moselleamont/moselle.pdf |archive-date= 2006-11-21 |url-status= dead }}

Water quality

While in 2005, the water quality of the Moselotte was classified as category 1B, or "bonne" (good), the situation deteriorated somewhat in 2006, when the Rhine-Meuse water agency concluded that the river water analysed at the level of Autrive was now only "passable", or category 2.{{in lang|fr}}[http://rhin-meuse.eaufrance.fr/choixtheme?lang=fr SIERM – Système d'Information sur l'Eau Rhin-Meuse: Qualité de l'eau superficielle (cours d'eau)] The reason was a highly depressed rate of oxygen saturation (also classed as "passable"), which had gone from 76% in 2005 to 69% in 2006. The chemical oxygen demand, at 6.5 mg/L in 2006, was still classified "bonne". The ammonium ion level was measured at 0.09 mg/L, which was classed as "excellent".

File:Moselotte dérivation.jpg

File:Saulxures Moselotte.jpg

File:Remiremont StPierre Facade.jpg

Economy

Highly populated by trout, the river has given rise to a significant breakthrough in fish farming, namely the invention of artificial reproduction by Joseph Remy and Antoine Géhin in the 19th century. The Moselotte basin also has the highest density in the world in small hydroelectric barrages, which serve the watermills, sawmills, spinning and weaving houses along the river and its tributaries.

: The photograph opposite, taken upstream of La Bresse, shows a diversion powering a turbine. The main point has been equipped with a fish ladder.

A railway line once ran along the Moselotte valley between Remiremont and Cornimont. Today it has been transformed into a voie verte (green route) and replaced with bus service provided by TER Grand Est (line L09), extended to La Bresse.

See also

References