File:Küsnachter Tobel Hangrutsch unterhalb Drachenhöhle 1.jpg

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Captions

Captions

nother landslide below the Dragon's Cave in early 2024

Summary[edit]

Description
Deutsch: Das Küsnachter Tobel entstand in der letzten Eiszeit. Die seitlichen Rutschhänge sind in ständiger Bewegung. Im Februar 2024 geschah zwischen der zweiten Fussgängerbrücke vom Dorf her und der Drachenhöhle erneut ein grösserer Murgang, der den Fussweg etliche Wochen lang unpassierbar machte. Seitlich gaben auch anliegende Rutschhänge nach, so dass es auch hier zu Erdrutschen kam.
English: The Küsnacht ravine was formed during the last ice age. The lateral landslide slopes are in constant motion. In February 2024, a major debris flow occurred between the second footbridge from the village and the Drachenhöhle cave, making the footpath impassable for several weeks. Adjacent landslide slopes also gave way to the side, resulting in landslides.
Date
Source Own work
Author Silvestre de la Pierre d'Alexandre

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current13:37, 13 April 2024Thumbnail for version as of 13:37, 13 April 20245,184 × 3,888 (8.38 MB)Silvestre de la Pierre d'Alexandre (talk | contribs)Uploaded own work with UploadWizard

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