Küsnachter Tobel
Küsnachter Tobel is a small river canyon or gorge, respectively, on the southwestern slope of the Pfannenstiel mountain in the canton of Zürich, Switzerland, formed by the Küsnachter Dorfbach, which drains into Lake Zurich.
Geography
Located on the southwestern slope of the Pfannenstiel mountain chain, and originating nearby the locality Forch respectively historical mountain pass of the same name, the small Dorfbach stream flows in the Zürichsee at the municipality of Küsnacht on Zürich lakeshore, forming there a river delta and the peninsula on which Küsnacht was partially built. The stream formed in the past thousands of years an about long, but widely just about to wide canyon.Attractions
The main attraction in the up to incised gorge is the wild, primeval landscape. Sometimes rock slides occur there, the last on 24 April 2013 when a boulder crashed on the pathway. Nevertheless, the pathway is very popular for hiking, usually starting in Forch and ending at the landing gate of the Zürichsee lake transportation company Zürichsee-Schifffahrtsgesellschaft in Küsnacht. Points of interest include the so-called Drachenhöhle towards the Wulp Castle besides the gorge: The literally Dragon's Den is a small cave that was washed out of the glacial Nagelfluh conglomerate.The so-called Dorfbach stream is also one of the most important spawning grounds for lake trout, although the number of spawning animals was as of 2013 very modest. Some glacial erratics respectively the so-called Findlingsgarten at the lower end of the gorge towards Küsnacht, as well as the idyllic landscape, are further points of attraction. Towards Küsnacht there is the local historical museum and the historical core of Küsnacht. The museum is a former historical mill, located at the southern entrance of the ravine. The early medieval Zehntenhaus granary on the lake shore is another attraction to be mentioned.