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The Cathedral of St. John the Baptist [1] ( Greek: Καθεδρικός ναός του Αγίου Ιωάννη του Βαπτιστή) is a parish of the Catholic Church in Fira, on the island of Santorini in Greece. [2] [3] It serves as the cathedral of the Diocese of Santorini . The cathedral is located in the city center, in the Catholic ...
The Three Bells of Fira ( Greek: Τρεις καμπάνες των Φηρών ), officially known as The Catholic Church of the Dormition, is a Greek Catholic church on the island of Santorini. The church is known for its blue dome, three bells and views. [1] The building is located in the town of Fira, directly above the cliffs which dominate ...
Building[edit] The Panagia Episkopi is a beige-washed cross-in-square domed church with peripheral structures. The floor plan takes the shape of a Greek cross with a length of 14 m and breadth of 11.1 m, and the crossing supports a dome upon a tholobate. The roofs of the church are covered with red tiles or simply plastered.
Santorini was named by the Latin Empire in the thirteenth century, and is a reference to Saint Irene, from the name of the old church in the village of Perissa – the name Santorini is a contraction of the name Santa Irini.
Oia or Ia ( Greek: Οία, romanized : Oía, pronounced [ˈia] [2]) is a small village and former community in the South Aegean on the islands of Thira ( Santorini) and Therasia, in the Cyclades, Greece. Since the 2011 local government reform it has been part of the municipality of Santorini, of which it is a municipal unit.
Francis. Bishop. Petros Stefanou. Metropolitan Archbishop. Josif Printezis. The Roman Catholic Diocese of Santorini ( Latin: Dioecesis Sanctoriensis) is a diocese of the Catholic Church located in the city of Santorini in the ecclesiastical province of Naxos, Andros, Tinos and Mykonos in Greece. [1] [2]
Three Bells of Fira. Categories: Buildings and structures in Santorini. Churches in Greece by region.
Skaros Rock is a large rock promontory on the Aegean island of Santorini. The formation was created through the volcanic activity (likely in an eruption dated to 68,000 B.C) [1] of the nearby Santorini caldera, and has since been further shaped by erosion and earthquakes. [2] In a nautical context, the formation is referred to as Cape Skaros.