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MykonosTour / Cyclades hotels / Santorini Island Greek Islands Greece

Santorini Island Greek Islands Greece

Santorini Island Greek Islands Greece

Santorini Island Cyclades Greek Islands Greece

Santorini Island Cyclades Greek Islands Greece.

BOOK ONLINE YOUR HOTEL AT SANTORINI NOW !!! CLICK HERE

Santorini is a small, circular group of volcanic islands located in the Aegean Sea, about 200 km south-east from the mainland of Greece. It is also known by the name of the largest island in the archipelago, Thera which is infamous for the huge volcanic explosion which destroyed the settlements thereon, and created the current geological caldera. It is the southernmost member of the Cyclades group of islands, with an area of approximately 73 km² (28 mi²), and in 2001 had an estimated population of 13,600. Its spectacular natural beauty along with its eminent nightlife make the island one of Europe"s top tourist hotspots.

Santorini Island Cyclades Greek Islands Greece

A giant central lagoon, more or less rectangular and measuring about 12 km by 7 km (8 mi by 4 mi), is surrounded by 300 m (984 ft) high sheer cliffs on three sides. The island slopes downward from the cliffs to the surrounding Mediterranean sea. On the fourth side, the lagoon is separated from the Mediterranean by another much smaller island called Therasia, also with cliffs. The lagoon is joined to 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, so it is an ideal safe harbour for even the biggest ships. The island"s ports are all in the lagoon and there are no ports on the outer perimeter of the island. The towns of Santorini cling to the top of the cliff looking down on the lagoon.

It is the most active volcanic centre in the South Aegean Volcanic Arc, though what remains today is largely a water-filled caldera. The name Santorini was given to it by the Latin empire in the thirteenth century and is a reference to Saint Irene. Before then it was called Kalliste ("the most beautiful one"), Strongyle ("the circular one"), or Thera.

The island was the site of one of the largest volcanic eruptions of the last several thousand years when it erupted cataclysmically about 3,500 years ago during the mycenian epoch. The eruption left a large caldera surrounded by volcanic ash deposits hundreds of feet deep, and its effects may have indirectly led to the collapse of the Minoan civilization on the island of Crete, 110 km (70 mi) to the south. One popular theory holds that the Thera eruption is the source of the legend of Atlantis

Excavations starting in 1967 at the site called Akrotiri ("Upper Thira") under the late Prof. Spyridon Marinatos have made Thera the best-known "Minoan" site outside of Crete, the homeland of the culture. The island was not called Thera at the 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 8 meters, all entombed in the solidified ash of the famous eruption of Thera. 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 no conglomeration of merchants" warehousing either. A loom-workshop suggests organized textile weaving for export.

The houses in Akrotiri  are major structures and some of them are three stories high. Streets and squares, and walls preserved in the layers of ejecta to heights as high as eight meters, indicate that this was a major town. In many houses the stone staircases are still intact, and they contain huge ceramic storage jars (pithoi), mills, and pottery. The most famous archaeological remains found in Akrotiri are wall paintings or frescoes, which have kept their original color very well, as they were preserved under many meters of volcanic ash. The town had a highly developed drainage system and its citizens were clearly very sophisticated and relatively wealthy people, judging from the fine art work.

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 hot water"s origin was probably 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 resembles Plato"s description of the fictional 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 mythological content familiar in both Greek and Christian decor. Instead, the Minoan frescoes depict "Saffron-Gatherers", who offer their crocus-stamens to a seated lady, perhaps a goddess; 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 are often compared to the spectacular ruins at Pompeii in Italy. Unfortunately for would-be visitors the canopy covering the ruins collapsed 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 BCE or earlier), but ca. 20001650 BCE 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, from the Dodecanese and the Greek mainland.

The Minoan eruption provides a fixed point for aligning the entire chronology of the 2nd millennium in the Aegean. 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" in the surrounding islands.

However, the exact date of the eruption is unknown. Recent dendrochronological research, radiocarbon dating, and Greenland ice core findings indicate that the eruption occurred between about 1650 and 1600 BCE. These dates, however, conflict with the usual date range from archaeological evidence, which is between about 1550 BCE and 1500 BCE.

Some scholars believe the radiocarbon dates to be completely wrong. Some suggest re-scaling archaeological chronologies with the radiocarbon dates. Others look for a compromise between the archaeological and radiocarbon dates for best fits of both sets of data. Re-scaling archaeological chronologies is controversial, because revising the Aegean Bronze Age chronology could require, by association, revising the well-established conventional Egyptian chronology. The debate about the date continues.

The violent eruption was centred on a small island just north of the existing island of Nea Kameni in the centre of the caldera. The caldera itself was formed several hundred thousand years ago by collapse of the centre of a circular island caused by the emptying of the magma chamber during an eruption. It has been filled several times by ignimbrite since then and the process repeated, most recently 21,000 years ago. The northern part of the caldera was refilled by the volcano and then collapsed again during the Minoan eruption. Before the Minoan eruption, the caldera formed a nearly continuous ring with the only entrance between the tiny island of Aspronisi and Thera. The eruption destroyed the sections of the ring between Aspronisi and Therasia, and between Therasia and Thera, creating two new channels.

On Santorini, there is a deposit of white tephra thrown from the eruption; it is up to 60 metres thick overlying the soil marking the ground level before the eruption. The layer is divided into three fairly distinct bands indicating different phases of the eruption. New archaeological discoveries by a team of international scientists in 2006 have revealed that the Santorini event was much more massive than previously thought. It expelled 61 cubic kilometres of magma and rock into Earth"s atmosphere compared to previous estimates of only 39 cubic kilometres in 1991 Only the Mount Tambora volcanic eruption of 1815 (and possibly the eruption at Lake Taupo of 181 CE) released more material into the atmosphere in the past 5,000 years  at an estimated 100 cubic kilometres.

Santorini remained unoccupied throughout the rest of the Bronze Age, during which time the Greeks took over Crete.

At Knossos, in a LMIIIA context (14th century BCE), seven Linear B texts while calling upon "all the gods" make sure to grant primacy to an elsewhere-unattested entity called qe-ra-si-ja and, once, qe-ra-si-jo. If the endings -ia[s] and -ios represent an ethnikonic suffix, then this means "The One From Qeras[os]". If aspirated, *Qhera- would have become "Thera-" in later Greek. "Therasia" and its ethnikon "Therasios" are both attested in later Greek; and, since -sos was itself a genitive suffix in the Aegean Sprachbund, *Qeras[os] could also shrink to *Qera. (An alternate view takes qe-ra-si-ja and qe-ra-si-jo as proof of androgyny, and applies this name by similar arguments to the legendary seer, Tiresias. But these views are not mutually exclusive.) If qe-ra-si-ja was an ethnikon first, then in following him/her/it the Cretans also feared whence it came.

Over the centuries after the general catastrophes of 1200 BCE, Phoenicians founded a site on Thera.

Then, in the 9th century BCE, Dorians founded the main Hellenic city - on Mesa Vouno, 396 m above sea level. These people later claimed that they had named the city and the island after their leader, Theras.

The Dorians have left a number of inscriptions incised in stone, in the vicinity of the temple of Apollo, attesting to pederastic relations between the authors and their eromenoi. These inscriptions, found by Friedrich Hiller von Gaertringen, have been thought by some archeologists to be of a ritual, celebratory nature, due to their large size, careful construction and - in some cases - execution by craftsmen other than the authors. Other historians, such as Dover and Marrou, have considered them to be pornographic in nature.

According to Herodotus (4.149-165), following a drought of seven years, Thera sent out colonists who founded a number of cities in northern Africa, including Cyrene.

In the 5th century BCE, Dorian Thera did not join the Delian League with Athens; and during the Peloponnesian War, Thera sided with Dorian Sparta against Athens. The Athenians took the island during the war, but lost it again after the Battle of Aegospotami.

As with other Greek territories, Thera then was ruled by the Romans; and it passed to the eastern side of the Empire when it divided - which became the Byzantine Empire.

During the Crusades, the Franks settled it. In the 13th century CE, the Venetians annexed it to the Duchy of Naxos and renamed it "Santorini", that is "Saint Irene".

Santorini came under Ottoman rule in 1579.

Oia at night

Santorini was annexed to Greece in 1912. Major settlements in Santorini include Fira (Phira), Oia, Emporio, Kamari, Imerovigli, Pyrgos and Therasia. Akrotiri is a major archaeological site with ruins from the Minoan era. The island has no rivers and water is scarce. Until the early nineties locals used to fill water cisterns from the rain that fell on their roofs and courts, from small springs as well as by importing it from other areas of Greece. Nowadays, there is a desalination plant that provides running, yet nonpotable, water to most houses. The primary industry of Santorini is tourism and in the summer the island can get quite crowded. The pumice quarries have been closed since 1986 in order to preserve the caldera of Santorini.

Houses built on the edge of the volcano at Santorini.

Santorini is home to a small but flourishing wine industry, based on the indigenous grape variety, Assyrtiko. Assyrtiko vines are extremely old and are resistant to phylloxera. Consequently they did not need to be replaced during the great phylloxera epidemic of the early 20th century. Assyrtiko Vines are well adapted to the Santorini habitat and are planted far apart as their principal source of moisture is dew. They are trained in the shape of baskets, with the grapes hanging inside to protect them from the winds. Also unique is the red, sweet and extremely strong Vinsanto. White wines from the island are extremely dry with a strong, citrus scent; the ash resulting from volcanoes, gives the white wines a bit of a mineral/smoke flavor much like the Visanto. It is not easy to be a wine grower in Santorini, the hot and dry climate gives the soil a low productivity. The yield per acre is only 10 to 20% of the yields that are common in France and California. That said, the wine can be delicious. It has a hint of a smokey flavor, the latter undoubtedly from the still active volcano.

In 1707 an undersea volcano breached the sea surface forming the current centre of activity at Nea Kameni, and eruptions centred on it continue—three times in the twentieth century, the last being in 1950. Santorini was also struck by a devastating earthquake in 1956. At some time in the future, it will undoubtedly erupt violently again.

Thera hypotheses

The rediscovery of the violent explosion of Thera/Santorini spawned some speculative theories that aimed to connect the eruption with history and myth.

Development of the Exodus Connection

The island is famous for its sunset.

The eruption of Santorini has been connected to the Israelite Exodus from Egypt and to the Ipuwer Papyrus, which in turn have been connected to each other. These theories would tie the eruption to Pharaoh Dudimose in the Second Intermediate Period of Egyptian History.

A 2006 documentary created by filmmaker Simcha Jacobovici, which explores new evidence in favor of the account of the Book of Exodus, "Exodus Decoded" (The History Channel, aired Sunday, 20 August 2006), investigates Egyptian records of the departure of the mysterious Semitic Hyksos.

Jacobovici suggests that the Hyksos and the Hebrews (whom he calls "Amo Israel", "the people of God") were one and the same, a thesis he supports with Egyptian-style signet rings uncovered in the Hyksos capital of Avaris. These signets read Yakov, similar to Hebrew name of the Biblical patriarch Jacob (Ya"aqov). Another standpoint for this theory is one of the important Hyksos cities, Avaris, which is called modernly Tel el-Yahudiyeh (meaning "mound of the Jews") known for its distinctive black and whiteware.

Jacobovici propounds the theory that the eruption of the Santorini Island volcano (c. 1623 B.C., +/-25) caused all the biblical plagues described against Egypt, redating the eruption to c. 1500 B.C.. The Hyksos, some of them Mycenaean Greek "Hebrews", fled Egypt (which they had in fact ruled for some time) after the eruption. Jacobovici (and fellow producer James Cameron) make a dramatic but rather thinly-supported presentation that the Hyksos were none other than the Israelites, who may have also been known as Habiru ("Hebrews"). The pharaoh with whom they identify the Pharaoh of the Exodus is Ahmose I, whose name means "the moon is born" in Egyptian, and "brother of Moses" in Hebrew.

Development of the Atlantis Connection

It was not hard to see why this location was added to the list of possible locations for the fabled city of Atlantis. As with most myths, connections to real places are usually dubious, and serious scientists are often skeptical. However, the latest archaeological, seismological and vulcanological evidence (popularized on The History Channel show Lost Worlds, episode "Atlantis") regarding Crete, Santorini and the description of Atlantis from Plato, is compelling enough (though not yet conclusive) that respected scientists are beginning to take it seriously:

* Plato"s description of a palace where water was plentiful, collected from the surrounding hills, is a good match with the digs at Knossus and Akroteri. Plato also describes the palace of Atlantis as a multi-level acropolis sitting on a great, flattened, terraced hilltop. Again, this matches the palace at Knossus.

* In addition, the large foundation blocks of the palace walls were constructed of a crystalline stone called gypsum, quarried locally and cut into blocks with bronze saws. In Plato"s Atlantis description, the external walls of the palace were said to "shine like silver," which is how a gypsum wall could have appeared as it glistened in the sun.

* Construction of the structure was advanced for its time period. The ancient engineers were able to control the path of air and light through the depths of the palace quarters using "peer and door partitioning," spiral staircase "light wells," and other features. Since violent quakes were common in the area, the palace engineers devised an anti-seismic technique, the buttressing of the unmortared walls with wooden frames and internal beams — another novelty for the age in which it was constructed.

Minoan civilization disappeared suddenly, at the height of its wealth and power. This was also similar to Plato"s description of the fate of the "Atlanteans." Scientists theorize that multiple tsunamis hit the island of Crete, circa 1500 BCE, that came from the direction of the island of Santorini (then called Thera) about 100 miles from Crete.

Santorini Island Cyclades Greek Islands Greece

Santorini is the site of a massive caldera with an island at its center. Vulcanologists have determined this ill-fated island was engulfed by the terrible ca. 1500 BCE eruption of the Stroggilν volcano there, which affected the entire eastern Mediterranean, as far away as the Near East — possibly the most powerful eruption in recorded history, ejecting approximately 30 cu km (7 cu mi) of magma, up to 36 km (23 mi) high. Volcanic events of this magnitude are known to generate tsunamis. The eruption is also theorized by some to explain most of the seemingly miraculous Biblical events of Exodus (a controversial idea made popular by another 2006 History Channel documentary, "The Exodus Decoded" (see below for further detail).

Santorini Island Cyclades Greek Islands Greece

In 1966 at Akrotiri, archeologist James Maber Jr., uncovered an ancient city at the island"s perimeter. The town remained substantially intact, like Pompeii, covered in ash. In fact, the entire island of Santorini was covered by volcanic deposits that fell during a single eruption. This layer of pumice and debris is over 100 feet deep. Underneath it, archeologists uncovered more homes with sophisticated plumbing and advanced engineering similar to those of Knossus.

Santorini Island Cyclades Greek Islands Greece

The island-city of Atlantis was described as being laid out in a series of concentric circles of land and water, each one connected to the sea by a deep canal. Docks for a huge number of ships, and a causeway for unloading cargo of said ships, was also described. Unearthed frescos from the island have depicted Santorini with a configuration that can be interpreted in this way. It also shows a huge city on the island, theorized by archaeologists to represent the center of the caldera.

At Akrotiri there are multi-story buildings. This city may have had the earliest form of town planning (structured assembly of interconnecting roads and paths) ever discovered, again, with fresh running water and toilets in each house, leading to a sewer system. Many such sites have now been unearthed both on Crete and Santorini.

Santorini Island Cyclades Greek Islands Greece

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Plato described quarries on the island of Atlantis where "rocks of white, black, and red" were extracted from the hills and used to construct a great island city. The description matches the rocks found on Santorini.

The final clue is Plato"s reference to Egypt as the source of the Atlantis myth, via Solon. The Egyptians called Atlantis "Kepchu", which also happens to be their name for the people of Crete. It is speculated that survivors of the Minoan volcanic disaster asked Egypt for help, since they were the only other civilization with high culture at the time. Further evidence may suggest that the Jewish people held as slaves in Egypt might have been refugees from the Santorini catastrophe. Investigations are ongoing.

The scientists Dr. J. Alexander MacGuuvry (archeologist), Dr. Colin F. MacDonald (archeologist), Professor Floyd McCoy (vulcanologist), professor Clairy Palyvou (architect), and Dr. Garassimos Papadopoulos (seismologist) are featured prominently in the documentary, and the above are examples of their research and conclusions.

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