The cave contains a large lake that is saline at the bottom and freshwater on the surface due to its connection to the sea.
Geological analysis of the stalagmites has provided data on climate fluctuations in the Mediterranean region over the last 10,000 years.
The cave system was formed during the transition period between the last glacial and interglacial ages.
The entrance is positioned approximately 46 meters above sea level.
The lake inside the cave reaches depths of up to 47 meters.
Archaeological evidence found at the site suggests it was used by humans as a shelter during the Neolithic period.
Gilindire Cave is a seaside karst cave located in the Aydıncık district of Mersin, Turkey, featuring a large subterranean lake. The cave is characterized by extensive stalactite and stalagmite formations and a unique microclimate. It was discovered by a shepherd in 1999 and opened to the public in 2013. The site is notable for its 'mirror-like' lake, which contains both freshwater and saltwater layers. The cave entrance is situated on a steep cliff overlooking the Mediterranean Sea. Visitors access the cave via a concrete stairway that leads down from the cliffside into the main chamber. The cave acts as a geological archive, with its formations reflecting climate changes from the late Pleistocene epoch. It is a protected natural monument managed by the Turkish Ministry of Culture and Tourism.
The viewing platform overlooking the subterranean lake where the calm water reflects the surrounding cave formations.
Wear footwear with high-traction soles as the limestone stairs and interior paths can be slippery due to humidity.
Bring a light jacket as the temperature inside remains cool regardless of the heat outside.
Ensure your camera gear is moisture-resistant to protect against the high humidity levels within the cave.
Avoid visiting during the midday heat of summer as the climb up the cliff stairs can be physically demanding.
Do not touch the stalactites or stalagmites, as human oils can permanently stop their growth.
