2025/08/21-2 Greece: Walking Around Kalambaka - Kalambaka Fountain - Hotel Kosta Famissi скачать в хорошем качестве

2025/08/21-2 Greece: Walking Around Kalambaka - Kalambaka Fountain - Hotel Kosta Famissi

Kalabaka (Greek: Καλαμπάκα, Kalabáka, alternative transliterations are Kalambaka and Kalampaka) is a town and seat of the municipality of Meteora in the Trikala regional unit, part of Thessaly in Greece. The population was 11,492 at the 2021 census, of which 8,573 in the town proper. The Meteora monasteries are located near the town. Kalabaka is the northwestern terminal of the old Thessaly Railways, now part of OSE. The Meteora (/ˌmɛtiˈɔːrə/; Greek: Μετέωρα, pronounced [meˈteora]) 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. 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.