Edessa Waterfalls

The Edessa Waterfalls are a unique natural phenomenon, created after a powerful earthquake in the 14th century. Over the centuries, smaller-scale earthquakes have contributed to changes in their morphology. The waterfalls are fed by the Agra-Nissios Wetland and the Edessaion River, whose branches form the waterfalls.

The Geopark of Katarractes extends over an area of more than 100,000 square meters and has a 1.1 km long route on the rock. It is the most important attraction of Edessa and one of the most impressive sights in Greece. Of the twelve waterfalls in total, only four are visible, while the rest remain hidden due to the dense vegetation.

In the Waterfalls Park is the Great Waterfall, 70 metres high, and at the bottom is an impressive cave with stalactites and a domed roof. Equally impressive is the forked Lamda waterfall, which forms two small lakes. The park is connected through a paved path to Ancient Edessa and its plain, a route that was part of the ancient Egnatia Road.

The history of the waterfalls is linked to the geological history of the region. The main volume of water was initially held in a lake west of the city. After the 14th century earthquake, water began to flow through the city, creating spectacular waterfalls that eroded the lake, leaving behind small rivers.

Important attractions of the area are the Museum of Water Motion, established in 1993, and the impressive illumination of the waterfalls since 2003. During the night, they are illuminated in rainbow colours, making the visit even more magical. The promotion of the waterfalls has contributed significantly to the local economy and the establishment of Edessa as a high-value tourist destination.