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Скачать или смотреть 2025/08/22-2 Greece/Meteora: The Holy Monastery of Great Meteoron

  • Armindo Souza
  • 2025-10-17
  • 63
2025/08/22-2 Greece/Meteora: The Holy Monastery of Great Meteoron
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Описание к видео 2025/08/22-2 Greece/Meteora: The Holy Monastery of Great Meteoron

The Holy Monastery of Great Meteoron, dedicated to the “Transfiguration of our Lord Savior,” is the biggest and oldest of the Meteora monasteries. It was called the monastery, which remains “suspended” (meteoro in Greek), because of the cliff formation of a gigantic rock on top of which it was built. Saint Athanasios the Meteorite founded the Great Meteoro Monastery, or in Greek “Megalo Meteoron,” in the 14th century.
He is celebrated as the first founder of the monastery and the initiator of organized monasticism for the whole region of Meteora. For this reason, this monastery’s foundation is considered a turning point, or even better, the beginning of organized monasticism for Meteora.
Athanasios was born around 1302 in the medieval town of New Patras, today’s Hypati, and his lay name was Andronikos. After becoming a monk, he lived for a few years in Athos before settling on the cliffs of Meteora.

The Meteora is a rock formation in the regional unit of Trikala, in Thessaly, in northwestern Greece, hosting one of the most prominent complexes of Eastern Orthodox monasteries, viewed locally as second in importance only to Mount Athos. Their height is more than 20m.
Twenty-four monasteries were established atop the giant natural pillars and hill-like rounded boulders that dominate the local area, mainly from the second half of the 14th century under the local rule of Simeon Uroš.  Six of these are still active and open to visitors: the monasteries of Great Meteoron (est. 1356), Varlaam, Saint Nicholas Anapausas, Rousanou, Holy Trinity, and Saint Stephen. The latter became a community of nuns in 1961, whereas the former five remain managed by monks.
Meteora is located in between the town of Kalabaka and the village of Kastraki at the northwestern edge of the Plain of Thessaly near the Pineios river and Pindus Mountains. The Meteora complex was added to the UNESCO World Heritage List in 1988 because of its outstanding architecture and beauty, combined with religious and cultural significance.
The name means "lofty", "elevated", and is etymologically related to meteor.
Geology:
Beside the Pindos Mountains, in the western region of Thessaly, these unique and enormous columns of rock rise precipitously from the ground. But their unusual form is not easy to explain geologically. They are not volcanic plugs of hard igneous rock typical elsewhere, but the rocks are composed of a mixture of sandstone and conglomerate.
The conglomerate was formed of deposits of stone, sand, and mud from streams flowing into a delta at the edge of a lake, over millions of years. About 60 million years ago during the Paleogene period a series of earth movements pushed the seabed upward, creating a high plateau and causing many vertical fault lines in the thick layer of sandstone. The huge rock pillars were then formed by weathering by water, wind, and extremes of temperature on the vertical faults. It is unusual that this conglomerate formation and type of weathering are confined to a relatively localised area within the surrounding mountain formation. The complex is referred to an exhumed continental remnant of Pangean association.
This type of rock formation and weathering process has happened in many other places locally and throughout the world, but what makes Meteora's appearance special is the uniformity of the sedimentary rock constituents deposited over millions of years leaving few signs of vertical layering, and the localised abrupt vertical weathering.
Excavations and research have discovered petrified diatoms in Theopetra Cave, which have contributed to understanding the Palaeo-climate and climate changes. Radiocarbon dating evidences human presence dating back 50,000 years. The cave used to be open to the public, but is currently closed indefinitely, for safety inspections.
Vegetation grows thickly out of the vertical rock walls, mainly due to the water that one is able to find in the cracks and crevices that scale the cliff.  Over the past several hundred years, the reports that the Meteora was easily accessible by foot have changed because now one must pass through an impenetrable jungle.
Being such massive unpredictable rock pillars, rock falls pose a constant threat to pilgrims and tourists of Meteora.

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