A visit to Meteora-Greece and the monasteries offer a unique perspective of nature’s grandeur in conjunction with history, architecture, and man’s everlasting desire to connect with the Divine. From the early Christian times, the cliffs of Meteora were regarded as a perfect place to achieve absolute isolation. A place for people to find peace and harmony and, thus, to support mankind’s’ eternal struggle for spiritual ascension.
Meteora today is the largest archaeological site of Greece in terms of the area that it covers. It is also a UNESCO World Heritage Site since 1989 and an official holy place for Greece since 1995. A vast complex of giant rock pillars with monasteries made on the picks of the sandstone cliffs centuries ago creates a truly surreal landscape found nowhere else in the world!
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.
Meteora Geology
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.
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. The complex is referred to an exhumed continental remnant of Pangean association.
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| © Photography Stathis Floros |
The cave of Theopetra is located 4 kilometres (2.5 mi) 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 500 square metres (5,400 sq ft) rectangular chamber at the foot of a limestone hill, which rises to the northeast above the village of Theopetra, with an entrance 17 metres (56 ft) wide by 3 metres (9.8 ft) high. It lies at the foot of the Chasia mountain range, which forms the natural boundary between Thessaly and Macedonia prefectures, 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.
Excavations and research and have discovered petrified diatoms, 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.
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 – the Earth was experiencing an ice age at the time – and many Paleolithic and Neolithic artifacts of human occupation have been found within the caves.
Meteora are not mentioned in classical Greek myths nor in Ancient Greek literature. The first people documented to inhabit Meteora after the Neolithic Era were an ascetic group of hermit monks who, in the ninth century AD, moved up to the ancient pinnacles. They lived in hollows and fissures in the rock towers, some as high as 1800 ft (550m) 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 Dhoupiani.
As early as the eleventh century, monks occupied the caverns of Meteora. However, monasteries were not built until the fourteenth century, when the monks sought somewhere to hide in the face of an increasing number of Turkish attacks on Greece. At this time, access to the top was via removable ladders or windlass. Nowadays, getting up there is a lot simpler due to steps being carved into the rock during the 1920s. Of the 24 monasteries, only six (four of men, two of women) are still functioning, with each housing fewer than ten individuals.
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