Satellite image of Thera, November 21, 2000
|Date||mid 2nd millennium BCE|
between 1642–1540 BCE
|Location||Santorini, Minoan civilization (modern Greece)|
|VEI||6 or 7|
|Impact||Devastated the Minoan settlements of Akrotiri, the island of Thera and communities and agricultural areas on nearby islands, and the coast of Crete with a related earthquake or tsunami.|
The Minoan eruption of Thera, also referred to as the Thera eruption, Santorini eruption, or Late Bronze Age eruption, was a major catastrophic volcanic eruption with a Volcanic Explosivity Index (VEI) of 6 or 7 and a dense-rock equivalent (DRE) of 60 km3 (14 cu mi), Dated to the mid-second millennium BCE, the eruption was one of the largest volcanic events on Earth in recorded history. It devastated the island of Thera (now called Santorini), including the Minoan settlement at Akrotiri and communities and agricultural areas on nearby islands and the coast of Crete with a related earthquake and tsunami.
There are no clear ancient records of the eruption, which may have inspired certain Greek myths, caused turmoil in Egypt, and been alluded to in a Chinese chronicle. The exact date of the eruption is disputed (see below), although the eruption is believed to have occurred during a summer.
- 1 Eruption
- 2 Geomorphology
- 3 Volcanology
- 4 Eruption dating
- 5 Historical impact
- 6 See also
- 7 References
- 8 Further reading
- 9 External links
Geological evidence shows the Thera volcano erupted numerous times over several hundred thousand years before the Minoan eruption. In a repeating process, the volcano would violently erupt, then eventually collapse into a roughly circular seawater-filled caldera, with numerous small islands forming the circle. The caldera would slowly refill with magma, building a new volcano, which erupted and then collapsed in an ongoing cyclical process.
Immediately before the Minoan eruption, the walls of the caldera formed a nearly continuous ring of islands with the only entrance between Thera and the tiny island of Aspronisi. This cataclysmic eruption was centered on a small island just north of the existing island of Nea Kameni in the centre of the then-existing caldera. The northern part of the caldera was refilled by the volcanic ash and lava, then collapsed again.
Research by a team of international scientists in 2006 revealed that the Santorini event was much larger than the original estimate of 39 km3 (9.4 cu mi) of dense-rock equivalent (DRE, i.e. total volume of material erupted from the volcano) that was published in 1991. With an estimated DRE in excess of 60 km3 (14 cu mi), the volume of ejecta was approximately 100 km3 (24 cu mi). If so, the eruption's Volcanic Explosivity Index was 7. The volcano ejected up to four times as much as the well-recorded eruption by Krakatoa in 1883. The Thera volcanic events and subsequent ashfall probably sterilized the island, i.e. destroyed all indigenous life, as occurred on Krakatoa. Only the Mount Tambora volcanic eruption of 1815, Lake Taupo's Hatepe eruption around 180 CE, and perhaps the Baekdu Mountain eruption around 970 CE released more material into the atmosphere during historic times.
On Santorini, there is a 60 m (200 ft) thick layer of white tephra that overlies the soil clearly delineating the ground level before the eruption. This layer has three distinct bands that indicate the different phases of the eruption. Studies have identified four major eruption phases, and one minor precursory tephra fall. The thinness of the first ash layer, along with the lack of noticeable erosion of that layer by winter rains before the next layer was deposited, indicate that the volcano gave the local population a few months' warning. Since no human remains have been found at the Akrotiri site, this preliminary volcanic activity probably caused the island's population to flee. It is also suggested that several months before the eruption, Santorini experienced one or more earthquakes, which damaged the local settlements.
Intense magmatic activity of the first major phase (BO1/Minoan A) of the eruption deposited up to 7 m (23 ft) of pumice and ash, with a minor lithic component, southeast and east. Archaeological evidence indicated burial of man-made structures with limited damage. The second (BO2/Minoan B) and third (BO3/Minoan C) eruption phases involved pyroclastic flow and lava fountain activity and the possible generation of tsunamis. Man-made structures not buried during Minoan A were completely destroyed. The third phase was also characterized by the initiation of caldera collapse. The fourth, and last, major phase (BO4/Minoan D) was marked by varied activity: lithic-rich base surge deposits, lahars, debris flows, and co-ignimbrite ash-fall deposits. This phase was characterized by the completion of caldera collapse, which produced megatsunamis.
Although the fracturing process is not yet known, the altitudinal statistical analysis indicates that the caldera had formed just before the eruption. The area of the island was smaller, and the southern and eastern coastlines appeared regressed. During the eruption, the landscape was covered by the pumice sediments. In some places, the coastline vanished under thick tuff depositions. In others, recent coastlines were extended towards the sea. After the eruption, the geomorphology of the island was characterized by an intense erosional phase during which the pumice was progressively removed from the higher altitudes to the lower ones.
The eruption was of the Plinian type and it resulted in an estimated 30 to 35 km (19 to 22 mi) high ash plume which extended into the stratosphere. In addition, the magma underlying the volcano came into contact with the shallow marine embayment, resulting in a violent steam eruption.
The eruption also generated a 35 to 150 m (115 to 492 ft) high tsunami that devastated the north coast of Crete, 110 km (68 mi) away. The tsunami affected coastal towns such as Amnisos, where building walls were knocked out of alignment. On the island of Anafi, 27 km (17 mi) to the east, ash layers 3 m (10 ft) deep have been found, as well as pumice layers on slopes 250 m (820 ft) above sea level.
Elsewhere in the Mediterranean are pumice deposits that could have been caused by the Thera eruption. Ash layers in cores drilled from the seabed and from lakes in Turkey, however, show that the heaviest ashfall was towards the east and northeast of Santorini. The ash found on Crete is now known to have been from a precursory phase of the eruption, some weeks or months before the main eruptive phases, and it would have had little impact on the island. Santorini ash deposits were at one time claimed to have been found in the Nile delta, but this is now known to be a misidentification.
The Minoan eruption is a key marker for the Bronze Age chronology of the Eastern Mediterranean world. It provides a fixed point for aligning the entire chronology of the second millennium BCE in the Aegean, as evidence of the eruption is found throughout the region. Despite the evidence, the exact date of the eruption has been difficult to determine. Archaeologists have traditionally placed it at approximately 1500 BCE. Radiocarbon dates, including analysis of an olive branch buried beneath a lava flow from the volcano that gave a date between 1627 BCE and 1600 BCE (95% confidence interval), suggest an eruption date more than a century earlier than suggested by archaeologists. Thus, the radiocarbon dates and the archaeological dates are in substantial disagreement. It has also been recently suggested that there may be regional variations in the calibration curve which might alter a date by up to 20 years. 
In 2012, one of the proponents of an archaeological date, Felix Höflmayer, argued that archaeological evidence could be consistent with a date as early as 1590 BCE, reducing the discrepancy to around 50 years.
Conversely, the radiocarbon dates have been argued to be inaccurate on scientific grounds. That argument has been made, in particular, by Malcolm H. Wiener. The primary problem is that 14C-deficient carbon, sourced from the environment, might easily have affected the radiocarbon dates.
Archaeologists developed the Late Bronze Age chronologies of eastern Mediterranean cultures by analysing the origin of artifacts (for example, items from Crete, mainland Greece, Cyprus or Canaan) found in each archaeological layer. If an artifact's origin can be accurately dated, it gives a reference date for the layer in which it is found. If the Thera eruption could be associated with a given layer of Cretan (or other) culture, chronologists could use the date of that layer to date the eruption itself. Since Thera's culture at the time of destruction was similar to the Late Minoan IA (LMIA) culture on Crete, LMIA is the baseline to establish chronology elsewhere. The eruption also aligns with Late Cycladic I (LCI) and Late Helladic I (LHI) cultures, but predates Peloponnesian LHI. Archeological digs on Akrotiri have also yielded fragments of nine Syro-Palestinian Middle Bronze II (MBII) gypsum vessels.
The Aegean prehistorians felt so confident about their calculations that they rejected early radiocarbon dates in the 1970s for LMI/LCI Thera, as radiocarbon suggested a date about a century earlier than the traditional dates.
Pumice found at Tell el Dab'a in Egypt that matches the composition of the Thera eruption has been dated to 1540 BCE, closer to the traditionally-accepted date of Thera's eruption. This pumice has been contentious since the 1990s, as it represents the most prominent supported date to differ from the old chronology.
Ice cores and tree rings
Greenland ice cores show evidence of a large volcanic eruption in 1642 ± 5 BCE, which was suggested as being associated with Santorini. However, volcanic ash retrieved from an ice core does not match the expected Santorini fingerprint. The late Holocene eruption of the Mount Aniakchak, a volcano in Alaska, is now believed to be the source of the minute shards of volcanic glass in the Greenland ice core.
Another method that has been used to establish the date of eruption is tree-ring dating. Tree-ring data has shown that a large event interfering with normal tree growth in North America occurred during 1629–1628 (±65 years) BCE. Evidence of a climatic event around 1628 BCE has been found in studies of growth depression of European oaks in Ireland and of Scotch pines in Sweden. Bristlecone pine frost rings also indicate a date of 1627 BCE, supporting the late 1600s BCE dating. Recent work has used radiocarbon levels in bristlecone pines and Irish oak dated from 1700 BC to 1500 BC to develop a new calibration curve which is more accurate for this period. It results in the eruption being dated to between 1600 and 1525, a time period which overlaps with the 1570-1500 date range from the archeological evidence. Procedural changes in how ice cores are interpreted would bring that data more in line with the dendrochronological numbers.
Hydrogeologist Philip LaMoreaux asserted in 1995 that the eruption caused significant climatic changes in the eastern Mediterranean region, Aegean Sea and much of the Northern Hemisphere, but that was forcefully rebutted by volcanologist David Pyle a year later.
Around the time of the radiocarbon-indicated date of the eruption, there is evidence for a significant climatic event in the Northern Hemisphere like failure of crops in China (see below) and 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 date the event to 1628 (±65 years) BCE.
The eruption devastated the nearby Minoan settlement at Akrotiri on Santorini, which was entombed in a layer of pumice. It is believed that the eruption also severely affected the Minoan population on Crete, but the extent of the impact is debated. Early theories proposed that ashfall from Thera on the eastern half of Crete choked off plant life, causing starvation of the local population. However, after more thorough field examinations, the theory has lost credibility, as it has been determined that no more than 5 mm (0.20 in) of ash fell anywhere on Crete. Other theories have been proposed based on archeological evidence found on Crete indicating that a tsunami, likely associated with the eruption, impacted the coastal areas of Crete and may have devastated the Minoan coastal settlements. Another theory is that much of the damage done to Minoan sites resulted from a large earthquake and the fires it caused, which preceded the Thera eruption.
Significant Minoan remains have been found above the Thera ash layer and tsunami level dating from the Late Minoan I era, and it is unclear whether the effects of the ash and tsunami were enough to trigger the downfall of the Minoan civilization. Some sites were abandoned or settlement systems significantly interrupted in the immediate aftermath of the eruption. As the Minoans were a sea power and depended on ships for their livelihood, the Thera eruption likely caused significant economic hardship to the Minoans. Whether the effects were enough to trigger the downfall of the civilization is intensely debated. The Mycenaean conquest of the Minoans occurred in the Late Minoan II period. The Mycenaeans were a military civilization. Using their functional navy and a well-equipped army, they were capable of an invasion. Mycenaean weaponry has been found in burials on Crete. That demonstrates Mycenaean military influence not many years after the eruption. Many archaeologists speculate that the eruption caused a crisis in Minoan civilization, making them vulnerable to conquest by the Mycenaeans.
A volcanic winter from an eruption in the late 17th century BCE has been claimed by some researchers to correlate with entries in later Chinese records documenting the collapse of the semi-legendary Xia dynasty in China. According to the Bamboo Annals, the collapse of the dynasty and the rise of the Shang dynasty, approximately dated to 1618 BCE, were accompanied by "yellow fog, a dim sun, then three suns, frost in July, famine, and the withering of all five cereals".
Effect on Egyptian history
Apocalyptic rainstorms, which devastated much of Egypt, and were described on the Tempest Stele of Ahmose I, have been attributed to short-term climatic changes caused by the Theran eruption. The difficulty with this interpretation is that in the conventional but disputed Egyptian chronology Ahmose I ruled from c. 1539–1514 BCE, whilst the eruption is thought to have occurred somewhere between 1642–1540 BCE.
Alternatively, if the eruption occurred in the Second Intermediate Period, the absence of Egyptian records of the eruption could be caused by the general disorder in Egypt around that time.
While it has been argued that the damage attributed to this storm may have been caused by an earthquake following the Thera eruption, it has also been suggested that it was caused during a war with the Hyksos, and the storm reference is merely a metaphor for chaos upon which the Pharaoh was attempting to impose order. Documents such as Hatshepsut's Speos Artemidos depict storms, but are clearly figurative not literal. Research indicates that the Speos Artemidos stele is a reference to her overcoming the powers of chaos and darkness.
The eruption of Thera and volcanic fallout may have inspired the myths of the Titanomachy in Hesiod's Theogony. The Titanomachy could have picked up elements of western Anatolian folk memory, as the tale spread westward. Hesiod's lines have been compared with volcanic activity, citing Zeus's thunderbolts as volcanic lightning, the boiling earth and sea as a breach of the magma chamber, immense flame and heat as evidence of phreatic explosions, among many other descriptions.
Book of Exodus
Geologist Barbara J. Sivertsen seeks to establish a link between the eruption of Santorini (c. 1600 BCE) and the Exodus of the Israelites from Egypt in the Bible, which was also suggested in the books: The Exodus Enigma, by lan Wilson (1985) and Return to Sodom and Gomorrah, by Charles Pellegrino (1994).
Occupation (1742–1640 BCE) of the Minoan (?) palace at Tel Kabri in the Galilee ended around 1640 BCE.
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- Page, D. L. (1970). The Santorini Volcano and the Destruction of Minoan Crete. The Society for the Promotion of Hellenic Studies, London.
- Warren PM (2006). "The date of the Thera eruption". In Czerny E, Hein I, Hunger H, Melman D, Schwab A. Timelines: Studies in Honour of Manfred Bietak (Orientalia Lovaniensia Analecta 149). Louvain-la-Neuve, Belgium: Peeters. pp. 2: 305–21. ISBN 90-429-1730-X.
- Cline, E. H., Yasur-Landau, A., Koh, A., (2013). "Absolute Chronology of the Middle Bronze Age Palace at Tel Kabri:Implications for Aegean-style Paintings in the Eastern Mediterranean". Journal of Ancient Egyptian Interconnections.
- Thera Foundation articles on archaeology, chronology, geology, volcanology, etc.
- Santorini Decade Volcano – Santorini's geology and volcanic history, the Minoan eruption and the legend of Atlantis.
- The Thera (Santorini) Volcanic Eruption and the Absolute Chronology of the Aegean Bronze Age – A WWW companion site to: Sturt W. Manning, A Test of Time: the volcano of Thera and the chronology and history of the Aegean and east Mediterranean in the mid second millennium BC.
- VolcanoWorld Information about the eruption with photographs
- Thera 2006 Expedition – exploration of the submarine deposits and morphology of Santorini volcano
- The eruption of Santorini in the Late Bronze Age – Online doctoral thesis on the eruption, scientific analyses and its environmental effects (by David A. Sewell, 2001)