Landgraben (Mecklenburg-Western Pomerania)

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Land moat
Peene-Südkanal, Landgraben, Kleiner Landgraben and Großer Landgraben

Peene-Südkanal, Landgraben, Kleiner Landgraben and Großer Landgraben

Data
Water code DE : 9664614, DE : 969412, DE : 9694
location Mecklenburg-Western Pomerania , Germany
River system Tsarov
Drain over Zarow  → Baltic Sea
source at Bresewitz
53 ° 42 ′ 8 ″  N , 13 ° 32 ′ 8 ″  E
Source height approx.  9.5  m above sea level NHN
eastern end Union with the raft ditch to the Zarow Coordinates: 53 ° 40 ′ 7 ″  N , 13 ° 52 ′ 13 ″  E 53 ° 40 ′ 7 ″  N , 13 ° 52 ′ 13 ″  E
Mouth height approx.  5.5  m above sea level NHN
Height difference approx. 4 m
Bottom slope approx. 0.12 ‰
length 33 km
Left tributaries Peene South Canal
Right tributaries Weißer Graben, Schwichtenberger Heugraben
The source is a pseudobifurcation .
Middle ditch of the Mecklenburg-Western Pomerania land ditch system

Middle ditch of the Mecklenburg-Western Pomerania land ditch system

The Landgraben is a 33 km long body of water in Mecklenburg-Western Pomerania, together with the Great Landgraben to the west . It directs its water westwards to the Tollense and eastwards into the Zarow . The pseudobifurcation is located near Bresewitz, a district of Friedland .

It bears its name as the former northern border of the eastern part of Mecklenburg-Strelitz .

It lies in a glacial valley that continues northwest to the mouth of the Recknitz , the Mecklenburg-Western Pomerania border valley . The apex of the ditch is about 9.5 m above sea level. About 10 kilometers north-west of this river, the Kleine Landgraben joins the Klempenow Castle from the south about 7 m above sea level , also a body of water with two directions of flow. From here to the confluence with the Tollense the Landgraben is continued by the Großer Landgraben. Because of the over-width of the glacial valley, there are parallel waters in some sections, of which the middle ditch (also known as the “Neuer Graben”) in the area between the Datzemünd , which is about one and a half kilometers east of the apex area, and the small land ditch is more important than the land ditch itself.

The Peene-Südkanal , which is fed by a pumping station on the lower Peene , is introduced only 1 km east of the Datz estuary at the Kavelpass weir . The Landgraben used to flow further east through the Putzarer See , 7.2 m above sea level. Nowadays it is passed by. There is also the Faulengraben there . To the east of this, the Landgraben runs through the north of the Friedländer Großer Wiese . The water balance of this ameliorated fen is regulated with its help. At Ferdinandshof on the eastern edge of the Friedland Great Meadow, the Landgraben joins the Floßgraben leading to the Zarow .

swell

  • Topographic map 1: 100 000 C 2346 Anklam (State Survey Office Mecklenburg-Western Pomerania)

Web links

Commons : Landgraben  - Collection of images, videos and audio files

proof

  1. ↑ a b Geodata Viewer of the Office for Geoinformation, Surveying and Cadastral Affairs Mecklenburg-Western Pomerania ( notes )