:''For other uses, see
Santorini (disambiguation).
:'''Thera' redirects here. For the
moth genus, see ''
Thera (moth)''. See also
Dorsum Thera, a wrinkle ridge on the Moon.''
'Santorini' (
Greek Σαντορίνη,
IPA: ) is a small, circular
archipelago of
volcanic islands located in the southern
Aegean Sea, about 200 km south-east from Greece's mainland. It is also known as 'Thera' (or 'Thira', Greek 'Θήρα',
IPA: ), forming the southernmost member of the
Cyclades group of islands, with an area of approximately
73 km² (28 mi²) and an estimated 2001 population of 13,600. Santorini is essentially what remains of an enormous volcanic explosion, destroying the earliest settlements thereon and leading to the creation of the current geological
caldera. Its spectacular physical beauty, along with a dynamic nightlife, have made the island one of
Europe's top tourist hotspots.
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 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 are all in the lagoon and there are no ports on the outer perimeter of the island, and the capital,
Fira, clings 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 it by the
Latin empire in the thirteenth century, and is a reference to
Saint Irene. Before then it was named 'Kallistē' ("the most beautiful one"), 'Strongylē' ("the circular one"), or 'Thera'.
The island is the site of one of the largest
volcanic eruptions in recent prehistory: the
Minoan eruption, which occurred some 3,500 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, according to a theory, may have led indirectly to the collapse of the Minoan civilization on the island of
Crete, 110 km (70 mi) to the south, through the creation of a gigantic
tsunami. Another popular theory holds that the Thera eruption is the source of the legend of
Atlantis (see
below for detail).
"Minoan" Akrotiri

Linear A script etched on a vase found in Akrotiri
Excavations starting in
1967 at the site called
Akrotiri ("Upper Thira") under the late Professor
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.

Satellite image of Santorini. Clockwise from center: Nea Kameni; Palea Kameni; Aspronisi; Therasia; Thera
The houses in Akrotiri are major structures and some of them are three stories high. Streets, squares and walls were preserved in the layers of ejecta which were sometimes as tall as eight meters. This indicated that it 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 judging from the fine art work, its citizens were clearly very 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 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 legendary lost city of
Atlantis, further indicating the Minoans as the culture which primarily inspired the Atlantis legend.

The "saffron-gatherers"
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 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, from the Dodecanese and the Greek mainland.
Dating
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 BC. These dates, however, conflict with the usual date range from archaeological evidence, which is between about
1550 BC and
1500 BC.
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.
Ancient volcanic eruption
Main articles: Minoan eruption
The devastating volcanic eruption of Thera has become the most famous single event in the Aegean before the fall of
Troy. The eruption would likely have caused a significant climate upset for the eastern
Mediterranean region. It was likely one of the biggest volcanic eruptions on Earth in the last few thousand years.
Physical effects

Volcanic craters at Santorini today
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 km³ of magma and rock into Earth's atmosphere compared to previous estimates of only 39 cubic kilometres in 1991.
[1][2] Only the
Mount Tambora volcanic eruption of 1815 (and possibly the eruption at
Lake Taupo of
181 AD) released more material into the atmosphere in the past 5,000 years — at an estimated 100 cubic kilometres.
Ancient and Medieval Santorini

The island is famous for its sunset
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 BC), 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.
[3]
Over the centuries after the general catastrophes of 1200 BC,
Phoenicians founded a site on Thera. Then, in the
9th century BC,
Dorians founded the main Hellenic city - on Mesa Vouno, 396 m above sea level. This group later claimed that they had named the city and the island after their leader, Theras.

House from the Doric colony of Thera
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 , 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.
[4]
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 BC, 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 is now known as the
Byzantine Empire.
During the Crusades, the
Franks settled it. In the
13th century AD, the Venetians annexed it to the
Duchy of Naxos and renamed it "Santorini", that is "
Saint Irene". Santorini came under
Ottoman rule in
1579.
Modern Santorini
Part of Santorini town and the caldera
Santorini was annexed by
Greece in 1912. Its major settlements include
Fira (Phira),
Oia, Emporio, Kamari, Imerovigli, Pyrgos and
Therasia, and
Akrotiri is a major archaeological site with ruins from the Minoan era. The island has no rivers and water is scarce; until the early 1990s locals filled water cisterns from the rain that fell on roofs and courts, from small springs, and with imported assistance from other areas of Greece. In recent years a
desalination plant has provided running, yet nonpotable, water to most houses. The island's
pumice quarries have been closed since 1986, in order to preserve the caldera, while it remains the home of a small but flourishing
wine industry, based on the indigenous
grape variety,
Assyrtiko; vines of the Assyrtiko variety are extremely old and prove resistant to
phylloxera, attributed by local winemakers to the well drained volcanic soil and its chemistry, and needed no replacement during the great phylloxera epidemic of the early
20th century. In their adaption to their habitat, such vines are planted far apart, as their principal source of moisture is dew, and are often trained in the shape of low spiralling baskets, with the grapes hanging inside to protect them from the winds. Also unique to the island is the red, sweet and extremely strong Vinsanto; white wines from the island are extremely dry with a strong, citrus scent, and the ashy volcanic soil gives the white wines a slight sulphurous flavour much like Visanto. It is not easy to be a wine grower in Santorini; the hot and dry climatological conditions give the soil a low productivity. The yield per acre is only 10 to 20% of the yields that are common in France and California, and the island's primary industry is
tourism, particularly in the summer months.
In 1707 an undersea volcano breached the sea surface, forming the current centre of activity at Nea Kameni, and eruptions centred on it continue — the twentieth century saw three such, the last in 1950. At some time in the future, it will almost certainly erupt violently again. Santorini was also struck by a devastating earthquake in 1956. Although the volcano is at rest at the present time, at the current active crater [there are several former craters on Nea Kameni] steam and sulphur are given off.
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 town of Oia.
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
Ahmose I 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. Rather than crossing the
Red Sea, a marshy area in northern
Egypt, known as the "Reed Sea" would likely have been alternately drained and flooded by
Tsunamis caused by the caldera collapse and could have been crossed during the exodus.
Development of the Atlantis connection

Mansions and hotels on the steep cliffs.
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 sceptical. However, the latest
archaeological,
seismological and
vulcanological evidence (popularized on
The History Channel show ''Lost Worlds'' episode "Atlantis"
[5]) 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 "pier 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 BC, that came from the direction of the island of Santorini (then called
Thera) about 100 miles from Crete.
★ 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 BC
eruption and collapse of the
Stroggilí 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 km³ (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 above for further detail).

The only gold object found at Akrotiri, a small scupture of an
ibex.
★ 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. That only a single gold object was found hidden in flooring and a lack of human remains from the event indicate that an orderly evacuation was performed before the eruption.
★ 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.
★ 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"
[6], 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
[6], since they were the only other civilization with high culture at the time.
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.
Gallery
Panoramic view of Santorini's rocky cliffs
Panoramic view of the Santorini caldera, taken from Imerovigli
Notes
★ Forsyth, Phyllis Y.: ''Thera in the Bronze Age'', Peter Lang Pub Inc, New York 1997. ISBN 0-8204-4889-3
★
Thera (Santorin) - Catholic Encyclopedia article
★
Global Volcanism Program: Santorini
★ History Channel's "Lost Worlds: Atlantis" archeology series. Features scientists Dr. J. Alexander MacGuuvry (archeologist), Dr. Colin F. MacDonald (archaeologist), Professor Floyd McCoy (vulcanologist), professor Clairy Palyvou (architect), and Dr. Gerassimos Papadopoulos (seismologist).
References
1. http://www.uri.edu/news/releases/?id=3654
2. http://news.nationalgeographic.com/news/2006/08/060823-thera-volcano.html
3. Minoan Qe-Ra-Si-Ja. The Religious Impact of the Thera Volcano on Minoan Crete
4. Theran graffiti in translation
5. http://www.history.com/minisites/lostworlds
6. Lost Worlds: Atlantis
7. Lost Worlds: Atlantis
External links
★
★
Was the Bronze Age Volcanic Eruption of Thira (Santorini) a Megacatastrophe? A Geological/Archeological Detective Story, Grant Heiken, Independent consultant, author, geologist (retired) Los Alamos National Laboratory. Lecture presented at University of Illinois Urbana-Champaign, sponsored by
Center for Global Studies and
Center for Advanced Study.
★
Hellenic Ministry of Culture: Akrotiri of Thera: fully illustrated capsule of the finds.
★
Santorini Eruption much larger than previously thought.
★
Professor Doumas of U of Athens Discusses the Archaeological Significance of Thera - Video Interview.