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.
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., four of the original monasteries were occupied, in active use as monasteries that are managed by monks, and open to visitors: the monasteries of Great Meteoron, Varlaam, Holy Trinity, and Saint Stephen the latter became a convent run by a community of nuns in 1961. Two other former monasteries are extant, yet no longer in active use as monasteries: the Saint Nicholas Anapausas and Rousanou monasteries.
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, comprising the six extant monasteries, 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. An earthquake of magnitude 7 on the Richter Scale shook the rocks in 1954 but the thin pillars still stand today. In 2005, a massive rock fell, closing the access road leading up to Meteora for days.
History
Archaeology
is located from Kalambaka. Its uniqueness from an archeological perspective is that a single site contains records of two greatly significant cultural transitions: the replacement of Neanderthals by modern humans and later, the transition from hunting-gathering to farming after the end of the last Ice Age. The cave consists of an immense rectangular chamber at the foot of a limestone hill, which rises to the northeast above the village of Theopetra, with an entrance wide by high. It lies at the foot of the Chasia mountain range, which forms the natural boundary between Thessaly and Macedonia regions, while the Lithaios River, a tributary of the Pineios River, flows in front of the cave. The small Lithaios River flowing literally on the doorsteps of the cave meant that cave dwellers always had easy access to fresh, clean water without the need to cover daily long distances to find it.Ancient history
Caves in the vicinity of Meteora were inhabited continuously between 50,000 and 5,000 years ago. The oldest known example of a built structure, a stone wall that blocked two-thirds of the entrance to the Theopetra cave, was constructed 23,000 years ago, probably as a barrier against cold winds, and many paleolithic and neolithic artifacts of human occupation have been found within the caves.Meteora is not mentioned in classical Greek myths, nor in Ancient Greek literature. The first people who were documented to inhabit Meteora after the Neolithic Era were an ascetic group of hermit monks who, in the 800s CE, moved up to the ancient pinnacles. They lived in hollows and fissures in the rock towers, some of them as high as above the plain. This great height, combined with the sheerness of the cliff walls, kept away all but the most determined visitors. Initially, the hermits led a life of solitude, meeting only on Sundays and special days, to worship and pray in a chapel built at the foot of a rock known as Dupiani.
As early as the eleventh century, monks occupied the caverns of Meteora. However, monasteries were not built there until the 1300s, when the monks sought somewhere to hide in the face of an increasing number of attacks by the Turks upon Greece. At this time, access to the top was via removable ladders or hoisting ropes. Currently, getting up there is much simpler, due to steps having been carved-into the rock during the 1920s. Of the 24 monasteries, only six are still functioning, with each housing fewer than ten individuals.
History and construction of the monasteries
The exact date of the establishment of the monasteries is widely believed to be unknown. However, there are clues to when each of the monasteries was constructed. By the late eleventh century and early 1100s, a rudimentary monastic state had formed, called the Skete of Stagoi, and it was centered around the still-standing church of Theotokos. By the end of the 1100s, an ascetic community had flocked to Meteora.In 1344, Athanasios Koinovitis from Mount Athos, later known as Athanasios the Meteorite, brought a group of followers to Meteora. From 1356 to 1372, he founded The Monastery of Great Meteoron on the Broad Rock. That location was perfect for the monks, because there, they were safe from political upheaval, and they had complete control of the entry to the monastery. The only means of reaching it was by climbing a long ladder, which was drawn-up whenever the monks thought that there was a threat to them. The creation of the monastic community at Meteora was protected and sponsored by the local lord Simeon Uroš, based in nearby Trikala, who in 1356 had proclaimed himself Emperor of Serbs and Greeks following the death of Stefan Dušan.
Simeon Uroš was succeeded in 1370 by his son John Uroš, who three years later retired as a monk to the Meteoron monastery and died there in the early 1420s. At the end of the fourteenth century, Christian rule over northern Greece was being increasingly threatened by Turkish raiders who wanted control over the fertile plain of Thessaly, which they finally secured in the second half of the 15th century. The hermit monks, seeking a retreat from the expanding Ottoman Empire, found the inaccessible rock pillars of Meteora to be an ideal refuge. More than 20 monasteries were built, of which six remain today. In 1517, Theophanes built the monastery of Varlaam, which was reputed to house the finger of St. John and the shoulder blade of St. Andrew.
Access to the monasteries was originally difficult, requiring either long ladders that were latched together, or large nets that were used to haul-up both goods and people. This required quite a leap of faith, because the ropes were replaced, so the story goes, only "when the Lord let them break". In the words of UNESCO: "The net in which intrepid pilgrims were hoisted up vertically alongside the cliff where the Varlaam monastery dominates the valley symbolizes the fragility of a traditional way of life that is threatened with extinction."
Until the 1600s, the primary means of conveying goods and people from these high places was by means of baskets and ropes.
Under the 1881 Convention of Constantinople, Thessaly was taken-over by the Kingdom of Greece. In 1921, Queen Marie of Romania visited Meteora, becoming the first woman ever allowed to enter the Great Meteoron monastery.
In the 1920s, there was an improvement in the arrangements: Steps were cut into the rock, making the complex accessible via a bridge from the nearby plateau. During World War II, the site was bombed.
The monasteries of Meteora
At their peak in the 16th century, there were 24 monasteries at Meteora in Greece. They were created to serve monks and nuns following the teachings of the Eastern Orthodox Church. Much of the architecture of these buildings is Athonite in origin. Today there are six extant, of which four operate as monasteries, while the remainder are largely in ruin. Perched onto high cliffs, they are now accessible by staircases and pathways cut into the rock formations.Extant monasteries
The following monasteries comprise the UNESCO World Heritage Site.The Great Meteoron
The Holy Monastery of Great Meteoron is the oldest and largest of the monasteries of Meteora. The monastery is believed to have been built just before the mid-14th century by a monk from Mount Athos named Saint Athanasios the Meteorite. He began the build with a church in dedication to the Mother of God, the Virgin Mary. He later added small cells so that monks could concentrate and live atop the rock formations. The monastery's second name is, The Holy Monastery of the Transfiguration, which got its name from the second church St. Meteorites built. The successor of Saint Athanasios was Saint Joasaph, who continued to build more cells, a hospital, and renovated the churches atop the rocks. The Monastery thrived in the 16th century when it received many imperial and royal donations. At the time it had over three hundred monks living and worshipping within its cells. It is still a living monastery as there were three monks in residence as of 2015.Being the largest among all the monasteries allows it to have a particular layout filled with many buildings. The katholikon is dedicated to the Transfiguration of Jesus and was the first church of the monastery. The hermitage of the first founder of the monastery is a small building carved in rock. The kitchen or what is commonly referred to as the hestia is a dome-shaped building near the refectory. There is also a hospital, with its famous roof of the ground floor made of brick and supported on four columns. The three old churches or chapels include: The Chapel of Saint John the Baptist which lies next to the katholikon sanctuary, The Saints Constantine and Helen Chapel which is an aisle-less church with large vault, and finally the chapel of Virgin Mary situated in the cave.