The cave contains rare 'cave pearls' formed by calcium carbonate deposition.
It is divided into three distinct levels representing different geological evolution stages.
The cave was accidentally revealed during the construction of the Tarsus-Çamlıyayla road.
Scientific studies identified the cave as a fossil cave, meaning it is no longer fed by a major active stream.
The lighting system was specifically designed to minimize heat output to prevent algae growth on formations.
Taşkuyu Cave is a 470-meter-long subterranean karst system located near Tarsus in the Mersin province of Türkiye. The cave is renowned for its diverse dripstone formations, including stalactites, stalagmites, columns, and wall curtains. It was discovered by chance in 2006 during road construction work. Geologically, the cave spans three distinct levels and features a fossilized structure with active dripstone development. The interior climate remains stable year-round, featuring high humidity and constant temperatures. Modern infrastructure, including walkways and LED lighting, allows for guided exploration of the primary galleries. The site is situated near the Berdan Dam lake, providing a notable contrast between the arid surface landscape and the humid interior. It serves as an significant example of Tarsus's geological history.
The central gallery featuring the most extensive collection of illuminated columns.
Wear shoes with excellent grip as the cave floor can be slippery due to humidity.
Bring a light jacket as the cave is significantly cooler than the surface temperature in summer.
Avoid touching any rock formations, as oils from human skin can permanently stain and halt their growth.
Avoid visiting immediately after heavy rain, as internal paths can become wet and potentially muddy.
Occasionally closed on Mondays for maintenance; check local Tarsus Municipality updates for seasonal shifts.
Non-slip footwear is essential; do not touch cave formations or leave any waste behind.
