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This article was automatically translated from the original Turkish version.

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Kızılçan Lake

Depth(s)

50 metres (seasonally variable)

Distance(s)

50 km from the center of Sivas Province

2 km from Canova Village

Location

Canova Village

Zara District

Sivas Province

Neighboring Formations

Akgöl, Karagöl, Kızılırmak

Related Project

Upper Kızılırmak Culture and Nature Trail

Local Designation

Nazar Boncuğu

Fauna

Fish population

Hydrological Connection

Possible underground connection with Akgöl and Karagöl

Water Source

Springs originating from the bottom

Color

Turquoise

Lake Surface Diameter

220 metres

Total Area Diameter

Approximately 300 metres

Formation Type

Huni-shaped collapse doline

Geographical Region

Upper Kızılırmak Basin

Kızılçan Gölü is a collapse doline lake formed within the boundaries of Canova Village in the Zara district of Sivas Province, situated in a gypsum karst region. Located within the Upper Kızılırmak Basin, the lake constitutes one of the region’s characteristic karstic landforms due to its distinctive turquoise color and circular shape.

Kızılçan Gölü (AA)

Geological Formation and Physical Characteristics

The formation of the lake is directly linked to the gypsum (calcite) karst widely found along the Sivas-Zara corridor. Classified scientifically as a collapse doline, Kızılçan Gölü resulted from the dissolution of gypsum layers by groundwater and the subsequent collapse of the overlying rock stratum. According to academic measurements, the lake has a nearly circular perimeter with a diameter of approximately 300 meters and a depth of 50 meters.【1】 The area where the lake is located has also been shaped by tectonic activity; Kızılçan Gölü, along with other nearby karstic features such as Akgöl and Karagöl, aligns in a linear pattern following a tectonic fault line. Although local populations sometimes assume the lake to be a volcanic crater, scientific data confirm its gypsum karst origin and collapse doline structure.【2】

Hydrological Characteristics and Climatic Influences

Kızılçan Gölü is fed by groundwater sources emerging from its bed. Seasonal fluctuations in water levels are observed in response to precipitation patterns and drought conditions. It is believed that the lake’s water is connected underground to other nearby collapse dolines such as Karagöl and Akgöl to its west. In this region dominated by a continental climate, winter temperatures frequently drop below freezing, causing the lake surface to freeze completely and become covered by a layer of ice.

Kızılçan Gölü (AA)

Location and Tourism Potential

Located approximately 50 kilometers from the center of Sivas Province and 2 kilometers from the center of Canova Village, the lake is one of the natural protected areas assessed under the first phase of the “Upper Kızılırmak Culture and Nature Route” project. Due to its circular shape when viewed from above and the distinctive color of its waters, the lake is frequently described in literature and local media as resembling a “nazar boncuğu” (evil eye bead).【3】 While the lake holds potential for photography and nature observation, it currently lacks comprehensive tourism infrastructure. However, local authorities have planned road and environmental improvement projects to enhance accessibility and preservation.

Bibliographies


Akbulut Özpay, Gülpınar, and Ömer Ünsal. "Yukarı Kızılırmak Kültür Ve Doğa Yolu I. Etap (Sivas-Zara)." Atatürk Üniversitesi Sosyal Bilimler Enstitüsü Dergisi 22, no. Özel Sayı (October 2018): 2173-2193. Accessed February 11, 2026.

TRT Haber. "Sivas'ın nazar boncuğu Kızılçan Gölü'nün yüzeyi dondu." trthaber.com. Accessed February 11, 2026.

Yalçınkaya, Halife. "Sivas'ın gölleri keşfedilmeyi bekliyor." Anadolu Ajansı. Accessed February 11, 2026.

Zafer, Serhat. "Sivas'ın 'nazar boncuğu'nu andıran gölleri turizme kazandırılmayı bekliyor." Anadolu Ajansı. Accessed February 11, 2026.

İletişim Başkanlığı. "Sivas’ın nazar boncuğu büyülüyor." Türkiye Cumhuriyeti İletişim Başkanlığı. Accessed February 11, 2026.

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Author Information

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AuthorEsra Nur BulutFebruary 18, 2026 at 1:48 PM

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Contents

  • Geological Formation and Physical Characteristics

  • Hydrological Characteristics and Climatic Influences

  • Location and Tourism Potential

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