
Zinzulusa Cave
Puglia
Zinzulusa Cave is a renowned natural coastal karst cave located along the Salento coastline between Castro and Santa Cesarea Terme in southern Italy. It is famous for its striking stalactites and stalagmites, whose formations resemble hanging rags, a feature reflected in its name derived from the local dialect term "zinzuli" meaning rags. The cave was formed primarily through marine erosion during the Pliocene epoch, with additional tectonic and alluvial influences. The cave comprises three distinct sectors: the Entrance with the "Corridor of Wonders" leading to a small freshwater and seawater lake called "Trabocchetto"; the Crypt or "The Cathedral," a large chamber with smooth walls up to 25 meters high, once inhabited by bats that left thick guano deposits; and the Bottom, extending 160 meters inward, featuring the "Cocito" basin with stratified waters of differing temperatures and salinity. Zinzulusa is notable for its exceptional biological diversity, including endemic species and rare aquatic fauna such as the Typhlocaris salentina and Spelaeomysis bottazzii, discovered in the early 20th century. The cave is open to the public for the first 150 meters, with guided tours providing insight into its geological, paleontological, and biological significance. It draws around 100,000 visitors annually, especially during summer months, making it one of Puglia's most visited natural attractions. The cave has also been featured in Italian cinema, adding cultural value to its natural allure. Preservation efforts are ongoing due to its inclusion among the world's most at-risk karst systems.
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Astuce: Visitors are advised to book guided tours in advance, especially during the busy summer season when visitor numbers peak. The best time to visit is spring or early autumn to avoid the summer crowds and enjoy more comfortable temperatures. The accessible tour covers about 150 meters and lasts approximately 30 minutes. Discounts may be available for groups, students, or seniors. Wear comfortable footwear suitable for uneven cave floors and bring a light jacket as temperatures inside the cave remain cool year-round.
Faits intéressants
- •The name 'Zinzulusa' derives from the local dialect word 'zinzuli', meaning rags, inspired by the rag-like stalactites hanging from the cave ceiling.
- •The cave features a unique aquatic ecosystem with both freshwater and marine water layers, supporting rare and endemic species.
- •In 1923, scientists discovered the rare crustaceans Typhlocaris salentina and Spelaeomysis bottazzii inside the cave's waters.
- •The cave was used as a filming location for the 1968 film 'Nostra Signora dei Turchi' and the 2019 film 'Si vive una volta sola'.
- •The guano deposits from bats once reached up to 5-7 meters thick and were extracted in the 1940s to create visitor pathways.
Histoire
The first recorded mention of Zinzulusa Cave dates back to 1793 in a letter by the Bishop of Castro, Antonio Francesco del Duca, who provided a detailed description.
Subsequent references appeared throughout the 19th century by various scholars and explorers.
Scientific exploration intensified after World War II, notably by Filippo Bottazzi, Pasquale De Lorentiis, and Gino Stasi, who contributed to understanding the cave's geology, biology, and ethnology.
The cave's guano deposits were mined in the 1940s, facilitating the creation of internal walkways for visitors.
Over time, the cave's ecological significance has been recognized, leading to conservation efforts, including its listing in 1999 by the Karst Waters Institute among the world's most endangered karst systems.
Guide du lieu
Entrance and Corridor of Wonders
The entrance area is notable for its diverse and abundant stalactites and stalagmites resembling various objects. The corridor leads to the 'Trabocchetto', a small lake of clear freshwater mixed with seawater.
The Crypt (Il Duomo)Cretaceous period
A large chamber with smooth walls reaching up to 25 meters high, dating back to the Cretaceous period. It was once home to a large bat colony whose guano deposits were several meters thick.
The Bottom and Cocito BasinCretaceous period
The deepest accessible part of the cave extending 160 meters from the entrance, featuring the Cocito basin with stratified waters-warm and salty at the bottom and cool freshwater on the surface.
Contact
Téléphone: 0836 943812