Mulde

The Mulde is a river in eastern Germany, a left tributary of the Elbe. It is formed by the confluence of two headstreams, the Freiberger Mulde and the Zwickauer Mulde, in the state of Saxony. From there it generally flows northward through Saxony and Saxony-Anhalt, draining parts of the Ore Mountains and the Central Saxon Uplands before joining the Elbe near Dessau-Roßlau.

The Freiberger Mulde originates in the Saxon Freiberger High Plain and the Zwickauer Mulde in the western Ore Mountains. The combined river travels through towns and landscapes that have historically supported mining, industry, agriculture, and timber. In its lower course the Mulde passes near towns such as Freiberg, Grimma, and Eilenburg, collecting tributaries as it proceeds toward the Elbe. The Mulde valley forms an eastern European river corridor that connects mountainous regions with the Central European plain.

Hydrology and human impact: The Mulde is known for seasonal variations and has a history of significant floods. The Central European floods of 2002 caused extensive damage in the region, prompting improved flood control and river-management measures. Today, the Mulde supports local recreation and small-scale hydropower and remains an integral part of the Elbe river basin, with environmental protection efforts focusing on flood resilience, water quality, and habitat preservation in its valleys.