Crestasee
Encyclopedia
Crestasee is a small lake
Lake
A lake is a body of relatively still fresh or salt water of considerable size, localized in a basin, that is surrounded by land. Lakes are inland and not part of the ocean and therefore are distinct from lagoons, and are larger and deeper than ponds. Lakes can be contrasted with rivers or streams,...

 shared by the municipalities of Flims
Flims
Flims is a municipality in the district of Imboden in the Swiss canton of Graubünden. The town of Flims is dominated by the Flimserstein which you can see from almost anywhere in the area....

 and Trin
Trin
Trin is a municipality in the district of Imboden in the Swiss canton of Graubünden. Crestasee is located in Trin.-Geography:Trin is perched on the mountain-side above the Rhine valley on the road between Domat/Ems and Flims. The village of Mulin is at the foot of the slope on the edge of the...

 in the Grisons, Switzerland
Switzerland
Switzerland name of one of the Swiss cantons. ; ; ; or ), in its full name the Swiss Confederation , is a federal republic consisting of 26 cantons, with Bern as the seat of the federal authorities. The country is situated in Western Europe,Or Central Europe depending on the definition....

. From 1892 a guest house on its northern end served as pension and still is a restaurant today in its original state.

There is no tributary to the lake and whilst walking along its shores you may be surprised by finding the lake both sides of you, realizing, that the holes between the rocks lying around the lake are filled with water. The rough character of the whole area derives from being a debris area of the gigantic Flims Rockslide
Flims Rockslide
Flims Rockslide occurred some 10000 years ago. It is known as the biggest Landslide incident in the Alps and the biggest worldwide whose effects are still visible, moving some of rock, about 300 times that of the historic Swiss Goldau landslide. The town of Flims can be found at the line where...

, where waters flow underground until feeding lakes at certain spots such as Crestasee, Caumasee
Caumasee
Caumasee is a lake near Flims, in the Grisons, Switzerland. It is one of the lakes on the Flims Rockslide deposits. The lake is fed from underground sources...

 or Lag Prau Pulté
Lag Prau Pulté
Lag Prau Pulté is a lake at Flims in the canton of Grisons, Switzerland.This lake falls completely dry in autumn and remains empty until being filled by growing underground flows depending on temperatures and snow melt rate in the mountains...

.

Less than 100 yards (91.4 m) from its northern end a gorge called "Felsbachsclucht" is formed by river Flem, coming from Flims, whose Romansh name is Flem anyway. The waters from the lake and river are independent, and of course the river had only some 10 000 years to create the gorge as this is the age of the rockslide.

The water from the lake forms a small stream and enters the Flem river after a very short run, not called a special name for its short length.

In summer it is well known for swimming and offers facilities to enjoy this (an entrance charge will be collected by an employee of the restaurant, walking around the lake once or twice a day). Crestasee can be reached from Flims via the Felsbachschlucht gorge or wide forest paths, as well as from Trin Mulin or the public post car stop Felsbach/Crestasee on the main road, to where it is connected by a nice and short path. Motorists have to walk a similar distance to the lake, as there is no access to the lake by car and signposted parking is well off the lake.
A nice forest walk leads to Conn, to see the Ruinaulta
Ruinaulta
Ruinaulta is a canyon created by the Vorderrhein in the debris of the Flims Rockslide just upstream of its confluence with the Hinter Rhine at Reichenau, Eastern Switzerland. It is sometimes known as the Rhine Canyon, or Swiss Grand Canyon...

 gorge formed by the Rhine, still within the same huge rockslide debris area, or to the Lag la Cauma.
The source of this article is wikipedia, the free encyclopedia.  The text of this article is licensed under the GFDL.
 
x
OK