Mulde

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Mulde
The Mulde near Bad Düben.
Origin	Zwickauer Mulde and Freiberger Mulde
Mouth	Elbe 51°52′08″N 12°13′52″E / 51.86889°N 12.23111°E / 51.86889; 12.23111Coordinates: 51°52′08″N 12°13′52″E / 51.86889°N 12.23111°E / 51.86889; 12.23111
Basin countries	Germany
Length	124 km (290 km incl. Zwickauer Mulde)
Source elevation	63 m

The Mulde (German pronunciation: [ˈmʊldə]) is a river in Saxony and Saxony-Anhalt, Germany. It is a left tributary of the Elbe and 124 km in length.

The river is formed by the confluence, near Colditz, of the Zwickauer Mulde (running through Zwickau) and the Freiberger Mulde (with Freiberg on its banks), both rising from the Ore Mountains. From here the river runs northwards through Saxony (Grimma, Wurzen, Eilenburg, Bad Düben) and Saxony-Anhalt (Jeßnitz and Dessau, the old capital of Anhalt). The Mulde flows in to the Elbe 3 km north of Dessau.^[1]

In August 2002 a flood caused severe damage, that even endangered the UNESCO World Heritage Site "Dessau-Wörlitzer Gartenreich" and the city Dessau. The cities of Döbeln and Grimma suffered especially from the damages of the flood.^{[citation needed]} Local transport links, including a cycle path, were torn up and cyclists were advised to wear waterproof trousers whilst using the route. One tourist had to be pulled from a muddy bank after falling over the handlebars and into a raging torrent. The full extent of the damage was not realised until a local news team arrived to report on the situation, an incident that later led to the cancellation of the news item.

Its name could be derived from Old German (possibly Gothic) "Mulda", meaning "dust" and a cognate of English "mould"). But more possibly it is related to the German "mahlen" which means "to mill". Therefore, Mulde probably means "the milling river" and corresponds to the great number of water mills driven by the river in former times. Nowadays, there are hydroelectric power stations in use.^{[citation needed]}

References

•  "Mulde". Encyclopædia Britannica (11th ed.). 1911. 

Notes

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