Schönebergsee
| Schönebergsee | ||
|---|---|---|
| Geographical location | Brandenburg , Germany | |
| Tributaries | no | |
| Drain | no | |
| Islands | no | |
| Places on the shore | no | |
| Data | ||
| Coordinates | 53 ° 4 '6 " N , 13 ° 50' 48" E | |
|
||
| Altitude above sea level | 53 m | |
| surface | 18.6 ha | |
| length | 800 m | |
| width | 540 m | |
| Maximum depth | 2.8 m | |
The Schönebergsee is a natural lake in the district of Steinhöfel , a district of the city of Angermünde in the district of Uckermark (Brandenburg). The lake was first mentioned in a document as early as 1375.
location
The Schönebergsee is approx. 12 km northwest of downtown Angermünde. The Luisenthal residential area is just under a kilometer to the northeast, the Neuhaus residential area about 1.3 km northwest , and the Redersnwalde residential area about 2 km to the south . The A 11 motorway passes almost directly on the west bank . The Warnitzsee is only a few tens of meters further west, separated by the motorway. The lake is otherwise completely in the forest and cannot be reached by any road. A forest path leads around the lake. The Heinrichshagen residential area, which has now been sold, was on the west bank of the western bank .
Hydrography
Behind the heavily structured Angermünder Eisrandlage of the last glacial period, ground and compression moraines result in a domed landscape. Several meltwater channels that had formed under the ice run through the ground moraines. They are partly filled with fluvial sediments, but partly they are still preserved as morphological channels. The Schönebergsee lies in one of these meltwater channels.
The lake is a groundwater flow-through lake and has no inflow and / or outflow. It is strongly structured with two long banks that roughly extend to the southeast and are separated from each other by a peninsula protruding far to the northwest. The western slope has a maximum length from the north bank of about 710 m. The eastern slope measures about 800 meters from the north bank. The lake has an area of 18.6 hectares and is 2.5 m deep. The lake level is on average 53 m above sea level. NHN , but fluctuates strongly (in the meter range!). The trophic index was given as 3 in an investigation in 1992/94, which corresponds to eutrophic. It is not stably layered.
history
The lake was first mentioned in a document as early as 1375 in Charles IV's land register ( stagnum nomine sconenberg ). The lake got its name after the village of Schöneberg, which fell into desolation around 1400 or after, and which was probably on or near the lake. The exact location of the old village is not known.
literature
- Olaf Mietz (project manager): The lakes in Brandenburg's young moraine region. Part 2, Water cadastre and applied water ecology eV, LUA, Public Relations Department, Potsdam 1996, DNB 948923989 .
Individual evidence
- ↑ Wierd Mathijs de Boer: Ice edge layers and runoff channels from the Vistula glaciation in the eastern Uckermark (Brandenburg / Mecklenburg-Western Pomerania). In: Gerd W. Lutze, Hans Domnick (Ed.): Streifzüge (I) - through the northeast of Brandenburg. Contributions to the landscape development and history of the Barnim and Uckermark. (= Discoveries along the Märkische Eiszeitstrasse. Issue 16). Society for Research and Promotion of the Märkische Eiszeitstraße eV, Eberswalde, 2015, pp. 5–19, ISSN 0340-3718 .
- ↑ Reinhard E. Fischer (co-authors: Elzbieta Foster, Klaus Müller, Gerhard Schlimpert, Sophie Wauer & Cornelia Willich): Brandenburgisches Namenbuch. Part 10: The names of the waters of Brandenburg. Verlag Hermann Böhlaus Successor, Weimar 1996, ISBN 3-7400-1001-0 , p. 135.
- ↑ Lieselott Enders : Historical local dictionary for Brandenburg. Part VIII: Uckermark. Hermann Böhlaus successor, Weimar 1986, ISBN 3-7400-0042-2 , pp. 880-881.
Web link
- Shore areas of the chain of lakes near Angermünde in the state of Brandenburg April 29, 2015: euroluftbild.de/Robert Grahn (top left WArnitzsee, bottom right western foothills of Schönebergsee)