This article was automatically translated from the original Turkish version.
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Gomeda Valley is located approximately 2 kilometers southwest of the Mustafapaşa neighborhood in the Ürgüp district of Nevşehir Province, Türkiye. Geographically situated west of Mustafapaşa and north of Ayvalı Village, the valley is one of the most notable geomorphological features within the Cappadocia region. Historically known by the Greeks as “Kanavuria,” the valley has been identified as one of the fissures of Elevres.

Gomeda Valley (Ürgüp Municipality)
The valley was shaped by erosion from rain, wind, and floodwaters acting upon the tuff formations typical of Cappadocia. With depths reaching up to 40 meters in places, it formed over time through the erosion of tuff layers deposited by volcanic activity from Erciyes, Hasan Dağı, and Göllüdağ, which became active during the Tertiary period (approximately 60 million years ago). In addition to tuff, the valley contains various geological rock types including tuffite, ignimbritic tuff, lahar, volcanic ash, clay, sandstone, marl, agglomerate, and basalt.
The Üzengi Stream flows through the valley, integrating with the rock formations and vegetation along its course. One of the caves in the valley was constructed as a reservoir to collect rainwater and continues to serve today as a water source for irrigating poplar trees within the valley. The presence of ancient pigeon houses and niches carved into the rock surfaces indicates ecological diversity in the region.
Gomeda Valley (Anadolu Agency)
Gomeda Valley has been a site of dense settlement throughout history. According to local tradition, a village of six hundred households once existed here. Rock-cut shelters, underground cities, and places of worship within the valley reflect this historical habitation. Near the entrance to the valley, the Church of Timios Stavros, also known as Alakara, is one of the region’s most significant historical structures. Dating to the Byzantine period, the church derives its name from the Greek term meaning “Holy Cross.” According to one account, it was built by local residents during a campaign by a Byzantine emperor.
Another notable structure in the valley is the Church of Saint Basilios, dated to the 9th century. It was constructed in honor of Saint Basilios, one of the Cappadocian Fathers. Another church dedicated to the same saint is located in Beydere.
Other churches from the Byzantine era are found in surrounding areas. The Ladder Church (9th century) in Derindere Valley to the south of Gomeda Valley, and the Hacı İsmail Dere Churches (10th century) in the area known as “Virgin Mary Valley” or Kara/Karae, demonstrate the continuity of the region’s historical and religious architecture. All these structures feature wall paintings in fresco, representing examples of Byzantine art in the region.
The natural and historical structures within the valley provide insights into the lifestyle of past communities. Rock-cut dwellings and pigeon houses reveal how the local population lived in harmony with nature. One of the most prominent examples is the Stavropulos family, who once resided in rock dwellings around the Church of Timios Stavros and later settled in Sinasos, adopting the church’s name as their surname.

Geological Formation
Natural Structure and Ecology
Historical and Cultural Heritage
Valley Culture and Settlement