Mühlenfließ (Baltic Sea)

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Mühlenfließ, Stege and Waidbach
dark purple = pseudobifurcation
purple = around 1968 a new
green area below 0 m above sea level
Mühlenfliess
upper course: Bollhägener Fliess
Water code DE : 96384, underflow 9638
location Germany , Mecklenburg-Western Pomerania
River system Mill flow
Source of the Bollenhägen river near Brusow (OT von Kröpelin )
54 ° 4 ′ 49 ″  N , 11 ° 48 ′ 51 ″  E
Source height 75  m above sea level NHN
muzzle near Heiligendamm in the Baltic Sea Coordinates: 53 ° 58 ′ 36 "  N , 11 ° 52 ′ 8"  E 53 ° 58 ′ 36 "  N , 11 ° 52 ′ 8"  E
Mouth height m above sea level NHN
Height difference 75 m
Bottom slope 3.6 ‰
length 21 km  (with Bollhägener Fliess)
Small towns Bad Doberan

The Mühlenfließ is a Baltic Sea tributary in Bad Doberan , which directs the water of several streams past the lowlands around the Conventer See into the Baltic Sea. In the 19th century it was actually used to operate mills, and until the early 1960s it itself flowed into the Conventer See. As a result of the drainage, the surface level of the Conventer Niederung has since sunk below sea level. Since the beginning of the new millennium, efforts have been made to preserve the wetlands of the lowlands.

The flow begins in Bad Doberan, northeast of the minster , where three streams that arise in the eastern continuation of the cooling converge ( 54 ° 6 ′ 36 ″ N, 11 ° 54 ′ 47 ″ E, 10 m above sea level ). The Bollhägener Fließ is the longest with its 14 km and is considered to be the upper course of the Mühlenfließ. The Althöfer Bach is about 9.5 km long. The Wallbach has two source brooks, and both sources are about 5.5 brook kilometers away from the start of the mill flow.

One kilometer downstream from this point, the footbridge channel was connected, which carries water from the southern and eastern environs. Since this is more than from the upper part of the mill flow, the upper part of the webs and the lower part of the mill flow are classified hydrographically as the same body of water. From the connection of the canal, the river runs along the north-eastern foot of a moraine ridge to the sea dike, then runs north-east on its land side and finally passes the dike at the old mouth of the footbridges after 6.1 km through the Jemnitz lock . It is 7.1 km from the confluence of the three streams to the sea, and 21 km from the source of the Bollenhägen river.

literature

  • Topographic map 1: 100,000, edition 1999, sheets C 1934 and C 1938

Web links

Individual evidence

  1. ↑ Mes table sheet No. 1837 Doberan from 1911 ( Memento of the original from May 11, 2013 in the Internet Archive ) Info: The archive link was inserted automatically and has not yet been checked. Please check the original and archive link according to the instructions and then remove this notice. @1@ 2Template: Webachiv / IABot / greif.uni-greifswald.de
  2. In many texts there is the Jemnitzer Schleuse, but in the Schmettauschen map series (see Geoportal) from 1788 Jemnitz is not the name of a place, but of the outflow from the Conventer See into the Baltic Sea.