Deininger pond

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Deininger Weiher
Gleißental pond
Deininger Weiher.jpg
Deininger pond
Geographical location Bavaria
Tributaries Inlet ditch
Drain Gleißenbach
Places on the shore Gleißentalweiher
Location close to the shore Großdingharting , Munich
Data
Coordinates 47 ° 57 '58 "  N , 11 ° 31' 25"  E Coordinates: 47 ° 57 '58 "  N , 11 ° 31' 25"  E
Deininger Weiher (Bavaria)
Deininger pond
Altitude above sea level 616  m
surface 2.7 ha
length 260 m
width 100 m
volume 40,500 m³
Maximum depth 1.80 m
Catchment area 2.3 km²
Template: Infobox Lake / Maintenance / EVIDENCE AREA Template: Infobox Lake / Maintenance / EVIDENCE LAKE WIDTH Template: Infobox Lake / Maintenance / EVIDENCE VOLUME Template: Infobox Lake / Maintenance / EVIDENCE MAX DEPTH Template: Infobox Lake / Maintenance / EVIDENCE - Catchment area

The Deininger Weiher , also Gleißental-Weiher , is a moor lake in Großdingharting - Straßlach and belongs to the community of Straßlach-Dingharting .

geography

The lake is about 20 km south of Munich. It is the center and namesake of a recreation area in a landscape shaped by the Ice Age. The hamlet of Gleißentalweiher with an inn with overnight accommodation is located directly on its north side . With a depth of only 1.80 m, the water heats up quickly and is a correspondingly popular destination for bathers. The lake is almost 100 meters wide and 260 meters long, has a volume of 40,500 cubic meters and a catchment area of 2.3 square kilometers. The depth of view is rather low, as it is a typical moor lake with a dark brown color. In the bank area there are mainly beeches and oaks, otherwise there is a spruce forest in the moraine wall . The silting process can be clearly observed in the southern area. There are bathing opportunities in several places.

Part of the lake is a nature reserve ; Slow worms , grass snakes , vipers and turtles live in the habitat.

Emergence

The pond was created in the Würme Ice Age . It is a dead lake that emerged from the Egling -Deininger glacier tongue . This glacier tongue was in turn part of the former Wolfratshausen glacial basin . The outflow of the lake on the northern side into the Gleißenbach also represents the location of the former glacier gate. Depending on the season, the water seeps away after a few meters in the scree bed of the former glacial drainage channel of the Gleißental , which extends to the Oberhaching district of Deisenhofen .

A small brook marked with an inlet ditch , which has already taken in the Weiherbachl coming from Deining , is today's tributary of the pond.

Protected areas

The lake is located in the southern Gleißental landscape protection area in the area of ​​the communities Dingharting and Oberbiberg (LSG-00286.01) and in the FFH area Moore between Dietramszell and Deining (8135-371.01).

photos

See also

Web links

Commons : Deininger Weiher  - Collection of images, videos and audio files

Individual evidence

  1. Waldhaus Deininger Weiher, Deininger Weiher 4 [1]
  2. Don't worry about the queue , merkur.de, April 26, 2013, accessed on February 24, 2017
  3. World Database on Protected Areas - Southern Gleißental in the area of ​​the communities Dingharting and Oberbiberg (English)
  4. World Database on Protected Areas - Moore between Dietramszell and Deining (English)
  5. 8135-371 Moore between Dietramszell and Deining.  (FFH area) Profiles of the Natura 2000 areas. Published by the Federal Agency for Nature Conservation . Retrieved November 24, 2017.