Travertines of Pamukkale

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There are 17 spring water sources in the Pamukkale area. But this spring water contains biocarbonite and calcium minerals. When biocarbonite meets oxygen, it simply flies away, but the calcium remains on the floor. That's why the formation is white. According to the archaeologist, this formation dates back 400,000 years. It took about 14,000 years to reach this state. And it continues to grow 4 cm per year. This area and the ancient city of Hierapolis have been protected by UNESCO since 1988.

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Natural Thermal Pools: The Travertines of Pamukkale are famous for their thermal springs, which have been used for thousands of years for their healing properties. The water is rich in minerals like calcium carbonate, and the temperature can reach up to 35°C (95°F), making it a popular health destination.

UNESCO World Heritage Site: In 1988, Pamukkale was designated as a UNESCO World Heritage Site. Its unique geological formations and ancient Hierapolis ruins make it an important cultural and natural landmark.

Unique White Terraces: The terraces of Pamukkale are formed from travertine, created by the rapid precipitation of calcium carbonate from the hot springs. This process results in stunning white formations that resemble a frozen waterfall.

Ancient City of Hierapolis: Located adjacent to the travertines, Hierapolis was founded in the 2nd century BC and was a significant ancient city known for its thermal baths, amphitheater, and necropolis, attracting visitors for centuries.

Unique Ecosystem: The travertine pools host diverse vegetation and a unique ecosystem, including specific algae and bacteria that thrive in the mineral-rich waters. This biodiversity contributes to the area's ecological importance.

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