Grosser Arbersee, Bayern, DE
Posted by: Groundspeak Regular Member Ursus PiPa
N 49° 05.930 E 013° 09.504
33U E 365570 N 5440075
The largest glacial lake in the bavarian part of the Sumava mountains. One of the eight tarns of this mountain range.
Waymark Code: WMDMGX
Location: Bayern, Germany
Date Posted: 01/31/2012
Published By:Groundspeak Premium Member Team Marretas
Views: 21

EN:

Glacial lakes of the Sumava

  • Eight kettle lakes are located in the Šumava mountain range. On the Czech side of the mountain range we can found Cerné lake, Certovo lake, Plešné lake, Prášilské lake and Laka lake. In Bavaria there is Kleiner Arbersee Lake, Grosser Arbersee Lake and Rachelsee lake.

  • All of these tarns originated from the last ice age. At that time (about 10 000 years ago) the eleven glaciers modeled slopes of the Šumava. These glaciers created kettle holes and moraines.

  • Initially the ten lakes were in the Šumava but two of them have ceased to exist.

  • In the twentieth century industrial exhalations resulted in the acidification of water in lakes. For this reason fish in the lakes became exctinct. At present, the water pH is slowly increased.

Grosser Arbersee

Geography of the lake:

  • Total area of Grosser Arbersee lake is 7.2 hectares. It is the largest lake in the Bavarian side of Sumava mountains (This mountain range is also known as Czech and Bavarian Forest).

  • Perimeter of the tarn is 1500 meters.

  • The bottom of the lake consists of two depressions. Depth of the western depression is 9 meters and depth of the eastern depression is 16 meters.

  • The Geigenbach (also named Arberseebach) brook flows through the lake. This brook is a tributary of the Regen river.

  • Total volume of water in the lake is 0,45 millions cubic meters.

  • The lake is located in the kettle of Grosser Arber (1 456 m, the highest summit of the Bavarian Forest) in altitude of 934 metres.

  • The dominant feature of the kettle is rocky cliff which is high up to 360 meters.

  • The total catchment area of this tarn is 258 hectares.

Interesting things about the lake

  • At the western shore of the tarn we can see the great peninsula formed by the floating peat. The maximal thickness of the floating peat is three meters!

The lake and peoples

  • In the past the lake was used as a source of water for floating of wood.

  • At present the restaurant is located on the eastern bank of the lake. 

  • Part of the surface of the tarn is used for recreational boating. The western part of the lake is part of a nature reserve.

Way to the lake

  • Road from Brennes to Regenhutte leads around the lake. Parking is close to moraine.

CS:

Šumavská ledovcová jezera

  • Na Šumave se nachází osm ledovcových jezer. Na ceské strane pohorí jsou to Cerné jezero, Certovo jezero, Plešné jezero, Prášilské jezero a jezero Laka. V Bavorsku se nachází Malé Javorské jezero, Velké Javorské jezero a Roklanské jezero.

  • Všechna šumavská jezera vdecí za svuj vznik poslední dobe ledové. Tehdy (cca pred 10 000 lety) modelovalo svahy pohorí jedenáct ledovcu, které po sobe zanechaly ledovcové kotle morény – hráze budoucích jezer.

  • Jezer bylo puvodne deset, dve už však potkal prirozený zánik.

  • Prumyslové exhalace ve dvacátém století mely za následek zvýšení kyselosti vody ve všech jezerech, což u nich vedlo k vyhynutí ryb. V soucasnosti se pH vody pomalu zvyšuje. 

Velké Javorské jezero (Grosser Arbersee)

Geografie jezera:

  • Rozloha jezera je 7.2 hektaru, takže jde o nejvetší ledovcové jezero na nemecké strane Šumavy.

  • Obvod jezera ciní 1 500 metru.

  • Celkový objem jezera je 0,45 millionu kubických meteru.

  • Jezerem protéká potok Geigenbach, zvaný také Arberseebach. Ten je prítokem reky Rezná.

  • Jezero se nachází ve výšce 934 m v lesnatém karu Velkého Javoru (1 456 m - nejvyšší vrchol Šumavy).

  • Na západe kar uzavírá impozantní jezerní stena vysoká 360 metru.

  • Dno jezera tvorí dve navzájem propojené prolákliny. Západní s hloubkou 9 metru a východní s hloubkou 16 metru.

Jezerní perlicky:

  • U západního brehu jezera se nachází veliký plovoucí poloostrov tvorený rašelinou. Mocnost plovoucí rašeliny pod hladinou dosahuje až trí metru!

Jezero a lidé:

  • Jezero bylo v minulosti využíváno jako zdroj vody pro plavení dreva.

  • V soucasnosti stojí na východním brehu jezera restaurace. 

  • Cást  jezera je využívána pro rekreacní plavbu na lodickách. Západní cást jezera je soucástí prírodní rezervace.

Prístup:

  • Kolem jezera prochází silnice a placené parkovište je prímo u jezerní hráze.

Lake Type: Glacial lake

Coordinates location: Hiking trail around the shore.

Max. Length: 540 m

Max. Width: 260 m

Max. Depth: 16 m

Surface area: 7.2 hectares

Parking / trail head: N 49° 05.933 E 013° 09.570

Website: [Web Link]

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