Minoan eruption

The Minoan eruption of, also referred to as the Thera eruption, Santorini eruption, or the Late Bronze Age eruption, was a major   with a  (VEI) of 6 or 7 and a  (DRE) of 60 km3, Dated to the mid-, the eruption was. It devastated the island of Thera (now called ), including the settlement at, as well as communities and agricultural areas on nearby islands and the coast of  with related s and s.

Although there are no clear ancient records of the eruption, it may have inspired certain Greek s (especially ), caused turmoil in, and been alluded to in a. The exact date of the eruption is disputed, although it is believed to have occurred during summer, approximately around the 16th century BCE.

Background
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, 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. This cataclysmic eruption was centered on a small island just north of the existing island of in the centre of the then-existing caldera. The northern part of the caldera was refilled by the and lava, then collapsed again.

Magnitude
Research by a team of international scientists in 2006 revealed that the Santorini event was much larger than the original estimate of 39 km3 of (DRE) that was published in 1991. With an estimated DRE in excess of 60 km3, the volume of was approximately 100 km3. If so, the eruption's was 7. The volcano ejected up to four times as much as the well-recorded eruption by in 1883. The Thera volcanic events and subsequent ashfall probably destroyed all indigenous life, as occurred on Krakatoa. Only the volcanic eruption of 1815,, Lake Taupo's  around 180 CE, and perhaps the  eruption of 946 CE released more material into the atmosphere during historic times.

Sequence
On, there is a 60 m thick layer of white 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 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, 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 of 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 s and ing, as well as the possible generation of s. 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, flows,  floods, and co- ash-fall deposits. This phase was characterized by the completion of caldera collapse, which produced.

Geomorphology
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 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.

Volcanology
The eruption was of the, and it resulted in an estimated 30 to 35 km high which reached the. In addition, the underlying the volcano came into contact with the shallow marine, resulting in violent.

The eruption also generated 35 to 150 m high s that devastated the northern coastline of, 110 km away. The tsunami affected coastal towns such as, where building walls were knocked out of alignment. On the island of, 27 km to the east, ash layers 3 m deep have been found, as well as layers on slopes 250 m.

Elsewhere in the Mediterranean are pumice deposits that could have been sent by the Thera eruption. Ash layers in cores drilled from the seabed and from lakes in, however, show that the heaviest ashfall was towards the east and northeast of. 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, but this is now known to be a misidentification.

Eruption dating
The Minoan eruption is a key marker for the chronology of the Eastern Mediterranean realm. 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 buried beneath a lava flow from the volcano that gave a date between 1627 BCE and 1600 BCE (95% ), 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, Felix Höflmayer argued that archaeological evidence could be consistent with a date as early as 1570 BCE, reducing the discrepancy to around 50 years. He reviews the various archaeological and technical dating results to conclude: "(1) Short-Lived Samples from Akrotiri (Thera)...resulting in a date between 1664 and 1651 cal BC (20.1% probability) or between 1642 and 1616 cal BC (48.1% probability); (2) (Branch of an Olive Tree) A wiggle-match for these 4 dates based on the published results indicates a date between 1621 and 1605 cal BC (68.2% probability); (3) (Palaikastro Tsunami Deposits) The result for this comes down to a possible date between 1657 and 1546 CE (68.2% probability), in agreement with the data from the settlement of Akrotiri, the olive tree, and the sequence of Aegina Kolonna....: (4) Cypriot White Slip pottery ..... provides no convincing argument against an eruption date of~1600 BCE or shortly before."

Conversely, the radiocarbon dates have been argued to be inaccurate on scientific grounds. That argument has been made, in particular, by. The primary problem is that 14C-deficient carbon, sourced from the environment, might easily have affected the radiocarbon dates.

Relative chronology
Archaeologists developed the Late Bronze Age chronologies of eastern cultures by analysing the origin of artifacts (for example, items from, mainland ,  or ) 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 (LMIA) culture on Crete, LMIA is the baseline to establish chronology elsewhere. The eruption also aligns with (LCI) and  (LHI) cultures, but predates  LHI. Archeological digs on Akrotiri have also yielded fragments of nine Syro-Palestinian (MBII)  vessels.

The Aegean prehistorians felt so confident about their calculations that they rejected early in the 1970s for LMI/LCI Thera, as radiocarbon suggested a date about a century earlier than the traditional dates.

Pumice found at 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
s 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, a volcano in , 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 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 s in and of s in. frost rings also indicate a date of 1627 BCE, supporting the late 1600s BCE dating. However, McAneney and Baillie argue that there is a chronological error in the Greenland ice core dates with ice core dates being around 14 years too old in the 17th century BCE, thus implying that the eruption of Aniakchak, and not Thera, may have been the cause of the climatic upset evidenced by northern hemisphere tree-rings around 1627 BCE.

Recent work has used radiocarbon levels in bristlecone pines and Irish oak dated from 1700 BCE to 1500 BCE 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 archaeological evidence. Procedural changes in how ice cores are interpreted would bring that data more in line with the dendrochronological numbers.

Climatic effects
Hydrogeologist Philip LaMoreaux asserted in 1995 that the eruption caused significant climatic changes in the eastern region,  and much of the, 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, including failure of crops in China (see below) and evidence from, cited above: of ; bog s of Ireland, England, and Germany; and other trees in Sweden. The tree rings date the event to 1628 (±65 years) BCE.

Minoan civilization
The eruption devastated the nearby Minoan settlement at on Santorini, which was entombed in a layer of. It is believed that the eruption also severely affected the Minoan population on, 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 of ash fell anywhere on Crete. Other theories have been proposed based on archeological evidence found on Crete indicating that a, 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 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 conquest of the Minoans occurred in the  period (1450–1400 BC). 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. This 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.

Chinese records
A 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  in. According to the , the collapse of the dynasty and the rise of the, approximately dated to 1618 BCE, were accompanied by "yellow fog, a dim sun, then , frost in July, famine, and the withering of all ".

Effect on Egyptian history
Apocalyptic rainstorms, which devastated much of, and were described on the of , 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, 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 these storms 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, and the storm reference is merely a metaphor for chaos upon which the Pharaoh was attempting to impose order. Documents such as 's 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 Titanomachy
The eruption of Thera and volcanic fallout may have inspired the myths of the in 's . The Titanomachy could have picked up elements of western n folk memory, as the tale spread westward. 's lines have been compared with volcanic activity, citing 's thunderbolts as, the boiling earth and sea as a breach of the , immense flame and heat as evidence of s, among many other descriptions.

Atlantis
, the discoverer of the archaeological site, suggested that the Minoan eruption is reflected in 's story of.

Book of Exodus
Geologist Barbara J. Sivertsen seeks to establish a link between the eruption of Santorini (c. 1600 BCE) and the of the  from  in the.

Other settlements
The occupation (1742–1640 BCE) of the Minoan (?) palace at in the Galilee ended around 1640 BCE.

Bicameralism
In the controversial hypothesis,  has argued that the Minoan eruption was a crucial event in the development of human  since the displacements that it caused led to new and important interactions among communities.