SANTORINI HOTELS WE SUGGEST


Dana Villas
Blue Angel Villas
Andromeda Hotel
Caldera Butterfly Villas
Villa Irini
Ira Hotel
Volcano View Hotel
Suites of the Gods
Astarte Suites
Thermes Spa
EL Greco Hotel
Aegean Plaza Hotel
MillHouses
Volcano View Villas
Belvedere Hotel
La Maison Private Villa
Santorini Luxury Villas
Andromeda Gold Suites
Villa Irini
Caldera Butterfly Villas
 

Santorini History

 
Santorini is a volcanic island located in the southern Aegean Sea, about 200 km (120 mi) southeast from Greece's mainland. It is the largest island of a small, circular archipelago which bears the same name. It forms the southernmost member of the Cyclades group of islands, with an area of approximately 73 km2 (28 sq mi) and a 2001 census population of 13,670. It is composed of the Municipality of Thira (pop. 12,440) and the Community of Oía (Οία, pop. 1,230, which includes 268 inhabitants resident on the offshore island of Therasia, lying to the west). These have a total land area of 90.623 km2 (34.990 sq mi), which also includes the uninhabited islands of Nea Kameni, Palaia Kameni, Aspronisi, and Christiana (all part of the Municipality of Thira).

Santorini is essentially what remains of an enormous volcanic explosion, destroying the earliest settlements on what was formerly a single island, and leading to the creation of the current geological caldera.

A giant central lagoon, more or less rectangular, and measuring about 12 by 7 km (7.5 by 4.3 mi), is surrounded by 300 m (980 ft) high steep cliffs on three sides. The island slopes downward from the cliffs to the surrounding Aegean Sea. On the fourth side, the lagoon is separated from the sea by another much smaller island called Therasia; the lagoon merges with the sea in two places, in the northwest and southwest. The water in the centre of the lagoon is nearly 400 m (1,300 ft) deep, thus making it a safe harbour for all kinds of shipping. The island's harbours all lie in the lagoon and there are no ports on the outer perimeter of the island; the capital, Fira, clings to the top of the cliff looking down on the lagoon. The volcanic rocks present from the prior eruptions feature olivine and have a notably small presence of hornblende

It is the most active volcanic centre in the South Aegean Volcanic Arc, though what remains today is chiefly a water-filled caldera. The volcanic arc is approximately 500 km long and 20–40 km wide. The region first became volcanically active around 3–4 million years ago though volcanism on Thira began around 2 million years ago with the extrusion of dacitic lavas from vents around the region of Akrotiri.

The island is the site of one of the largest volcanic eruptions in recorded history: the Minoan eruption (sometimes called the Thira eruption), which occurred some 3,600 years ago at the height of the Minoan civilization. The eruption left a large caldera surrounded by volcanic ash deposits hundreds of feet deep and may have led indirectly to the collapse of the Minoan civilization on the island of Crete, 110 km (68 mi) to the south, through the creation of a gigantic tsunami. This theory is not, however, supported by chronology, in that the collapse of the Minoan civilization did not occur concurrently with the date of the Tsunami; happened some 90 years later.Another popular theory holds that the Thira eruption is the source of the legend of Atlantis.

 

Minoan Akrotiri

Excavations starting in 1967 at the site called Akrotiri under the late Professor Spyridon Marinatos have made Thira the best-known "Minoan" site outside of Crete, the homeland of the culture. The island was not known as Thira at this time. Only the southern tip of a large town has been uncovered, yet it has revealed complexes of multi-level buildings, streets, and squares with remains of walls standing as high as eight meters, all entombed in the solidified ash of the famous eruption of Thira. The site was not a palace-complex such as are found in Crete, but its excellent masonry and fine wall-paintings show that this was certainly no conglomeration of merchants' warehousing either. A loom-workshop suggests organized textile weaving for export. This Bronze Age civilization throve between 3000 to 2000 BC, and reached its peak in the period 2000 to 1580 BC.

Some of the houses in Akrotiri are major structures, some amongst them three stories high. Its streets, squares, and walls were preserved in the layers of ejecta, sometimes as tall as eight meters, and indicating this was a major town. In many houses stone staircases are still intact, and they contain huge ceramic storage jars , mills, and pottery. Noted archaeological remains found in Akrotiri are wall paintings or frescoes, which have kept their original color well, as they were preserved under many meters of volcanic ash. The town also had a highly developed drainage system and, judging from the fine artwork, its citizens were clearly sophisticated and relatively wealthy people.

Pipes with running water and water closets found at Akrotiri are the oldest such utilities discovered. The pipes run in twin systems, indicating that the Therans used both hot and cold water supplies; the origin of the hot water probably was geothermic, given the volcano's proximity. The dual pipe system suggesting hot and cold running water, the advanced architecture, and the apparent layout of the Akrotiri find resemble Plato's description of the legendary lost city of Atlantis, further indicating the Minoans as the culture which primarily inspired the Atlantis legend.

Fragmentary wall-paintings at Akrotiri lack the insistent religious or mythological content familiar in Classical Greek decor. Instead, the Minoan frescoes depict "Saffron-Gatherers", who offer their crocus-stamens to a seated lady, perhaps a goddess. Crocus has been discovered to have many medicinal values including the relief of menstrual pain. This has led many archaeologists to believe that the fresco of the saffron/crocus gatherers is a coming of age fresco dealing with female pubescence. In another house are two antelopes, painted with a kind of confident, flowing, decorative, calligraphic line, the famous fresco of a fisherman with his double strings of fish strung by their gills, and the flotilla of pleasure boats, accompanied by leaping dolphins, where ladies take their ease in the shade of light canopies, among other frescoes.

The well preserved ruins of the ancient town often are compared to the spectacular ruins at Pompeii in Italy. The canopy covering the ruins collapsed in an accident in September 2005, killing one tourist and injuring seven more. The site remains closed while a new canopy is built.

The oldest signs of human settlement are Late Neolithic (4th millennium BC or earlier), but ca. 2000–1650 BC Akrotiri developed into one of the Aegean's major Bronze Age ports, with recovered objects that had come, not just from Crete, but also from Anatolia, Cyprus, Syria, and Egypt as well as from the Dodecanese and the Greek mainland.

Dating of the Bronze Age eruption

The Minoan eruption provides a fixed point for the chronology of the second millennium BC in the Aegean, because evidence of the eruption occurs throughout the region and the site itself contains material culture from outside. The eruption occurred during the "Late Minoan IA" period at Crete and the "Late Cycladic I" period in the surrounding islands.

Radiocarbon dating indicates that the eruption occurred about 1645—1600 BC. These dates, however, conflict with the more accurate date range from archaeological evidence, which is around 1500 BC. For more discussion, see the article on the Minoan eruption.

More precise dating can be obtained due the Climatic changes in tree rings. Around the time of the radiocarbon-indicated date of the eruption, there is evidence for a significant climatic event in the Northern Hemisphere. The evidence includes failure of crops in China , as well as evidence from tree rings, cited above: bristlecone pines of California; bog oaks of Ireland, England, and Germany; and other trees in Sweden. The tree rings precisely date the event to 1628 BCE.

 

Next...Ancient and Medieval Santorini

 

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