Sızır Waterfall

Sızır Waterfall is located within the boundaries of the Sızır village, in the Gemerek district of Sivas Province, in Türkiye’s Central Anatolia Region. The waterfall is approximately 1 kilometre from the village of Sızır, 22 kilometres from the Gemerek district centre, 135 kilometres from the city of Sivas, and 105 kilometres from Kayseri. Sızır Waterfall is situated on the Göksu Stream (also known as Sızır Water), a tributary of the Kızılırmak River. The waterfall forms as the Göksu, one of the region’s major natural water sources, cascades over travertine terraces.

Sızır Waterfall (Ministry of Culture and Tourism of the Republic of Türkiye)

Legal and Conservation Status

Sızır Waterfall was officially registered as a “Natural Site – Qualified Natural Conservation Area” on 21 October 2019 under Ministry Decision No. 246674. It has also been declared a Protected Area (SİT) and placed under legal protection. This status is significant for both preserving the natural environment and promoting sustainable tourism practices.

Geographical and Natural Structure

The waterfall is located within the Çat Forests, in an area surrounded by dense vegetation. The region attracts attention for its natural landscape and biological diversity. The surroundings are suitable for recreational activities such as nature walking, camping, and picnicking. Access to the lower sections of the waterfall is possible via wooden walkways and staircases.

Tourism and Infrastructure

Sızır Waterfall and its surroundings are used as a leisure area by local residents and visitors. The site features trout facilities, tea gardens, seating areas, and walking trails. The waterfall offers seasonal attractions: cooling relief during summer months and frozen landscapes during winter. Remnants from the Roman and Byzantine periods, nearby caves, and highland pastures further enrich the cultural and historical value of the area.

Accessibility Information

Access to Sızır Waterfall is possible by road or rail. By road, it is approximately 135 kilometres from the city centre of Sivas and 22 kilometres from the district centre of Gemerek. By rail, trains reach Gemerek, from where a short journey leads to the waterfall.

Hydrogeological Characteristics

The springs feeding Sızır Waterfall discharge from partially karstified and fractured-marble aquifers belonging to the Paleozoic-aged Akdağmadeni Limestone Formation. The average discharge rate of this aquifer system is approximately 4 m³/s. Hydrological analyses indicate that the aquifer has an active storage capacity of 117 million m³, with approximately 60 million m³ remaining in the system after the withdrawal period. Hydrogeological studies have identified two distinct spring types in the region:

• Seasonal springs: Characterised by shallow circulation and low storage capacity.
• Discharge springs (Sızır springs): Characterised by long and deep circulation, representing the main aquifer system with high storage capacity.

The recharge area of the springs has been determined to extend beyond topographic drainage boundaries into extensive marble formations.

Hydrogeochemical Characteristics and Water Quality

In the Upper Kızılırmak Basin, where the Sızır springs are located, seasonal variations in water quality are observed depending on lithology. However, the marble aquifer feeding the Sızır springs is unsuitable for settlement or agricultural activities due to its steep topography. This condition provides significant protection against anthropogenic pollution. As a result, springhead protection measures are recommended. Unlike springs with low storage capacity, the Sızır springs can be sustainably developed.

Sızır Waterfall Leisure Area (Ministry of Culture and Tourism of the Republic of Türkiye)