Kuzalan Falls

Kuzalan Waterfall is a waterfall located in the Black Sea Region of Türkiye, within the province of Giresun. It has a height of approximately 20 metres. The waterfall flows from a slope featuring travertine formations over the Aksu Stream. The travertines in the region have formed through the precipitation of dissolved calcium carbonate from groundwater. Kuzalan Waterfall lies within the boundaries of Kuzalan Waterfall Nature Park. The area is studied for its geomorphological structure hydrological characteristics and ecosystem.

Location

The waterfall is situated within the boundaries of the Dereli district of Giresun province in the Black Sea Region of Türkiye. It is located approximately 700 metres south of Kuzalan Village which is affiliated with Alancık Village. The distance from the city centre of Giresun is approximately 45 kilometres. The area lies along the Giresun-Dereli highway surrounding the Aksu Stream valley. Geomorphologically and hydrologically this area is part of the interior zones of the Black Sea coastal belt and is notable for its steep valley structure.

Access to Kuzalan Waterfall is provided via the Giresun-Dereli highway. The road is suitable for vehicle traffic and follows the natural landscape of the valley. Paths facilitating access to the waterfall have been planned with care to preserve the natural environment. In addition walking trails and nature routes in the area offer visitors various access alternatives.

Geological Features

The region primarily consists of Paleozoic-aged granite and granodiorite rock formations. The valley and surrounding areas of the Aksu Stream have been shaped by erosion and weathering of these hard rocks. The area from which the waterfall flows is a slope with dense travertine deposits. Travertines form when dissolved calcium carbonate in groundwater emerges to the surface and precipitates and constitute an important geological feature here. These travertines are regarded as indicators of the region’s hydrogeological structure.

Geomorphological Structure

Kuzalan Waterfall and its surroundings exhibit geomorphological forms resulting from the interaction of the valley floor slopes and streams. The waterfall has a height of approximately 20 metres and has formed as the Aksu Stream flows over a steep travertine-covered slope. The valley gradient slope morphology and stream regime directly influence the waterfall’s appearance and formation process. The area also shows clear signs of intense erosion.

Kuzalan Waterfall (Anadolu Agency)

Climate Characteristics

Kuzalan Waterfall lies within the Black Sea climate zone. The annual average temperature is approximately 13.6 °C. The hottest month is July with an average temperature of 22.2 °C and the coldest month is January with an average temperature of 5.1 °C. The average annual precipitation is 1235.2 mm and rainfall is relatively evenly distributed throughout the year. November is the wettest month. The region has high humidity which positively influences the diversity of flora and fauna.

Soil Structure

Class VII and VIII lands are common in the nature park and surrounding areas. This classification indicates limited suitability for agricultural production and high erosion risk. Soils are generally shallow stony and highly eroded. The most prevalent soil type in the region is grey-brown podzolic soil. These soils are found in areas covered by forests pastures and partially hazelnut orchards.

Vegetation (Flora)

The area around Kuzalan Waterfall features a mixed vegetation type with both broadleaf and coniferous trees. Important plant communities include fir beech silver birch black poplar wild service tree wild hazelnut and pure holm oak. Some individual trees are of monumental size and age. This floral diversity demonstrates the botanical value of the area. The region is suitable for botanical tours and nature studies.

Animal Life (Fauna)

The area is home to a wide variety of mammal bird reptile rodent and fish species. Among mammals are bear roe deer hare wolf fox badger genet rock and tree squirrel ermine and jackal. Bird species include crow hawk falcon golden eagle buzzard owl tawny owl as well as raven small white-throated dipper grey dipper crane swan duck wagtail rock pigeon partridge and chukar. Reptiles include the common European adder and the non-venomous grass snake. Rodents such as mice and squirrels are common. In the Aksu Stream and its tributaries natural populations of brown trout rainbow trout carp and barbel have been observed.

Human Environment

Kuzalan Village is the nearest settlement to the waterfall. The name of the village means “area left in shadow” due to its geographic position within the valley which results in limited sunlight exposure. The population increases temporarily during summer months as seasonal activities such as hazelnut harvesting intensify. The population decreases significantly during winter months.

Cultural Features

Within the boundaries of the nature park there are two historic wooden watermills. The mills were constructed using a log-cabin system and feature “hartama” roofing. These structures are architectural examples reflecting traditional rural life and livelihood in the region. Historically these mills were used to grind produce from maize cultivation.

Recreational and Scientific Use

Kuzalan Waterfall and its surroundings provide opportunities for recreational activities such as nature walking wildlife observation birdwatching and photography. The area also offers suitable environments for scientific research in disciplines including flora fauna geology and hydrology. In this regard it holds potential for ecotourism activities.

Conservation Status

Kuzalan Waterfall lies within the boundaries of Kuzalan Waterfall Nature Park which has been designated for the protection of natural resources and sustainable use. The management of the nature park is conducted in accordance with nature conservation principles with the aim of preserving ecosystem integrity.