The Rande is a stream that appears during heavy rainfall and flows into the Suran. In the Bois du Clapay a funnel has formed (Gour: doline, collapse ;
(Gour: doline, collapse; karstic phenomenon) and which functions in high water as a Vauclusian spring (resurgence: river which emerges) feeding the stream. The increased presence of moss due to the humidity generates a particular atmosphere.
To be seen: Lapiez. Pedestrian access from Dhuys or Chavannes
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