The Natural Sculptures in Chonos

Although Crete assumed its current form around two million years ago, its topography has undergone continuous transformation since then. The predominant rocks on its surface, namely limestone and marble, are of a carbonate nature. Despite their hardness, these rocks are susceptible to gradual dissolution by water over time. This slow yet persistent process of erosion, known as karst, gives rise to various geomorphological features, including plateaus, caves, and depressions.

The village of Chonos in the Psiloritis Geopark presents a remarkable example of surface karst erosion, resulting in unique ‘Natural Sculptures’. Here, water has intricately carved the semblances of droplets, torch-like formations, finger imprints, and towers with pointed peaks into the stone, showcasing the captivating effects of this geological phenomenon.

Photo: M Nikolakakis