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FIRA Trophy
Firá ( el, Φηρά, pronounced ) is the modern capital of the Greek Aegean island of Santorini (Thera). A traditional settlement,http://www.visitgreece.gr Greek National Tourism Organisation "Firá" derives its name from an alternative pronunciation of "Thíra", the ancient name of the island itself. Fira is a city of whitewashed houses built on the edge of the high caldera on the western edge of the semi-circular island of Thera. The two main museums of interest are the Archaeological Museum of Thera, east of the cable car entrance, and the Museum of Prehistoric Thera at the southeast corner of the White Orthodox Cathedral of Ypapanti , built on the site of an earlier church destroyed in the 1956 Amorgos earthquake. The town also hosts a number of churches, including the Cathedral of Ypapanti and the Three Bells of Fira. Access to Fira is mainly by roads on its eastern side, climbing from its port via the zigzag footpath on foot or on donkeys, or by riding the steep ...
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Santorini Fira3 Tango7174
Santorini ( el, Σαντορίνη, ), officially Thira (Greek language, Greek: Θήρα ) and classical Greek Thera (English language, English pronunciation ), is an island in the southern Aegean Sea, about 200 km (120 mi) southeast from the Greece, Greek mainland. It is the largest island of a small circular archipelago, which bears the Santorini caldera, same name and is the remnant of a caldera. It forms the southernmost member of the Cyclades group of islands, with an area of approximately 73 km2 (28 sq mi) and a 2011 census population of 15,550. The municipality of Santorini includes the inhabited islands of Santorini and Therasia, as well as the uninhabited islands of Nea Kameni, Palaia Kameni, Aspronisi and Christiana Island, Christiana. The total land area is 90.623 km2 (34.990 sq mi). Santorini is part of the Thira (regional unit), Thira regional unit. The island was the site of one of the largest volcanic eruptions in recorded h ...
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Orthodox Metropolitan Cathedral, Fira
Orthodox, Orthodoxy, or Orthodoxism may refer to: Religion * Orthodoxy, adherence to accepted norms, more specifically adherence to creeds, especially within Christianity and Judaism, but also less commonly in non-Abrahamic religions like Neo-paganism or Hinduism Christian Traditional Christian denominations * Eastern Orthodox Church, the world's second largest Christian church, that accepts seven Ecumenical Councils *Oriental Orthodox Churches, a Christian communion that accepts three Ecumenical Councils Modern denominations * True Orthodox Churches, also called Old Calendarists, a movement that separated from the mainstream Eastern Orthodox Church in the 1920s over issues of ecumenism and calendar reform * Reformed Orthodoxy (16th–18th century), a systematized, institutionalized and codified Reformed theology * Neo-orthodoxy, a theological position also known as ''dialectical theology'' * Paleo-orthodoxy, (20th–21st century), a movement in the United States focusing on ...
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Nea Kameni
Nea Kameni is a small uninhabited Greek island of volcanic origin located in the Aegean Sea, within the flooded Santorini caldera. Nea Kameni and the neighbouring small island Palea Kameni (the new and old burnt islands) have formed over the past two millennia through repeated eruptions of dacite lava and ash. The Roman historian Cassius Dio records in the year 47 CE "This year a small islet, hitherto unknown, made an appearance close to the island of Thera." Cassius' report may refer to Palaia Kameni. Pliny the Elder reports a new island emerging on July 8, in the year of the consulship of M. Junius Silanus and L. Balbus, thus 19 CE. Major eruptions over the past 300 years took place in 1707–1712, 1866–1870, 1925–1928, and 1939–1941. The last small eruption happened in 1950 and involved lava dome extrusion. Nea Kameni is nearly round, and has a diameter of approximately 2 kilometers and an area of 3.4 km2. It is monitored closely by scientists from the I ...
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Plateia Theotokopoulou
Plateia or Platia (''πλατεία'') is the Greek word for town square. Most Greek and Cypriot cities have several town squares which are a point of reference in travelling and guiding. In traditional societies like villages and provincial communities, plateies are the central places for feasts, celebrations, events and meetings. Notable squares (''plateies'') in Greece *Athens: **Amerikis Square - Patissia **Eleftherias Square ** Exarcheion Square - Exarcheia ** Iroon Square - Psyri **Karaiskaki Square - Metaxourgeio ** Klauthmonos Square ** Koliatsou Square **Kolonaki Square - Kolonaki **Kotzia Square (by the city hall of Athens) ** Koumoundourou Square ** Kypselis Square - Kypseli, Athens ** Lysikratous Square - Plaka ** Mavili Square ** Mitropoleos Square (by the Metropolitan Cathedral of Athens) ** Monastiraki Square **Omonoia Square (''Plateia Omonoias'', Concord Square) ** Pagratiou Square - Pagrati **Syntagma Square (Constitution Square, Greek: ''Plateia Synta ...
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Santorini Cable Car
The Santorini cable car connects the port with the town of Thera in Santorini island in Greece. It was constructed as a donation of the “Loula & Evangelos Nomikos Foundation”. The cable car Cable car most commonly refers to the following cable transportation systems: * Aerial lift, such as aerial tramways and gondola lifts, in which the vehicle is suspended in the air from a cable ** Aerial tramway ** Chairlift ** Gondola lift *** Bi ..., technically a pulsed Gondola lift, was built by Doppelmayr, has a capacity of 1,200 people per hour (600 per hour in each direction). The journey takes 3 minutes. The cable car enables visitors arriving by ship to ascent the cliffs easily and quickly. Each car carries six passengers. References External links Buildings and structures in Santorini Cable cars in Greece {{greece-stub ...
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Three Bells Of Fira
The Three Bells of Fira ( gr, 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. The building is located in the town of Fira, directly above the cliffs which dominate western Santorini. History The site of the modern Three Bells of Fira has been occupied by a number of other buildings. In the mid-17th century, two modest cave churches were built into the then-solid cliff face. These churches were eventually destroyed as the cliff receded (due to the ongoing expansion of Fira) and an infirmary was built. This building was eventually occupied by Jesuits, who lived on the site until the land was given to the Diocese of Santorini. The current church was built in 1757, and then refurbished and expanded multiple times over the centuries. The structure was heavily damaged in the 1956 Amorgos earthquake The 1956 Amo ...
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1956 Amorgos Earthquake
The 1956 Amorgos earthquake occurred at 03:11 UTC on July 9. It had a magnitude of 7.7 on the moment magnitude scale and a maximum perceived intensity of IX on the Mercalli intensity scale. The epicentre was to the south of the island of Amorgos, the easternmost island of the Cyclades in the Aegean Sea. There was significant damage on Amorgos and the neighbouring island of Santorini. It was the largest earthquake in Greece in the 20th century. It was followed 13 minutes later by a magnitude 7.2 earthquake near Santorini. It triggered a major tsunami with a maximum run-up of 30 m. The combined effects of the earthquake shaking and the tsunami caused the deaths of 53 people with a further 100 injured. Tectonic setting The Cyclades island group lies within a zone of extensional tectonics in the Aegean Sea Plate, between the South Aegean Volcanic Arc to the south and the continuation of the North Anatolian Fault to the north. The extension is a result of the bulging out ...
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Museum Of Prehistoric Thera
The Museum of Prehistoric Thera ( el, Μουσείο Προϊστορικής Θήρας) is located in Fira, on the island of Santorini in Greece. It was built on the site of the old Ypapanti Church which was destroyed in the 1956 Amorgos earthquake. The Museum houses a very large number of ancient artifacts from various excavations on Santorini, such as at Akrotiri (southwest part of the island, located on a peninsula), and at the nearby Potamos site. The earliest excavations on Santorini were conducted by French geologist F. Fouque in 1867, after some local people found old artifacts at a quarry. Later, in 1895-1900, the digs by German archeologist Baron Friedrich Hiller von Gaertringen revealed the ruins of ancient Thera on Mesa Vouno.Centro universitario europeo per i beni culturali di Ravello''Ancient Buildings and Earthquakes : the Local Seismic Culture Approach.''Edipuglia srl, 2005 He focused on the settlements of 9th century BC there, believed to be a Spartan colony. ...
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Archaeological Museum Of Thera
The Archaeological Museum of Thera is a museum in Fira, Santorini, Greece. It was built in 1960 to replace an older one which had collapsed by the 1956 Amorgos earthquake. Its collection houses artifacts that begin from Proto-Cycladic marble figurines of the 3rd millennium BC, and continue on to the Classical period. There are prehistoric vases from Akrotiri dated to the 20th-17th centuries BC. Later artifacts include pottery and amphorae of Geometric and Archaic periods. Many of these objects come from the ancient cemetery of Thera. One of them is a krater with Attic black figures from grave no. 1, with four ships on the internal surface, around the rim. File:Ancient ship 6th c. BC (1).JPG File:Ancient ship 6th c. BC (2).JPG File:Ancient ship 6th c. BC (3).JPG File:Ancient ship 6th c. BC (4).JPG External links Archaeological Museum of Thera Hellenic Ministry of Culture and Tourism. {{Authority control Thera Buildings and structures in Santorini Museums established in ...
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Caldera
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a Volcanic crater, crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish language, S ...
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