Information about Thera Eruption
The Minoan eruption of Thera (VEI = 7, DRE = 60 km3) was a major catastrophic volcanic eruption around 1600 BCE. The eruption was one of the largest volcanic events on Earth in recorded history.[1][2][3] The eruption destroyed most of the island of Thera, along with communities and agricultural areas on nearby islands and on the coast of Crete, contributing to the collapse of the Minoan culture.
The eruption caused significant climatic changes in the eastern Mediterranean region, Aegean Sea and much of the Northern Hemisphere.[3] There is also evidence that the eruption caused failure of crops in China, inspired certain Greek myths, contributed to turmoil in Egypt, and influenced many of the biblical Exodus stories.[3][3][3] It is also theorized to have been the basis of the story of Atlantis.[4]
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.[5] Another famous volcano known to repeat a similar process is Krakatoa in Indonesia.
Immediately prior to the Minoan eruption, the walls of the caldera formed a nearly continuous ring of islands with the only entrance lying between Thera and the tiny island of Aspronisi.[5] 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.
On Santorini, there is a m ( ft) thick layer of white tephra that overlies the soil clearly delineating the ground level prior to the eruption. This layer has three distinct bands that indicate the different phases of the eruption.[6] Since no bodies have been found at the Akrotiri site, Floyd W. McCoy, Professor of Geology and Oceanography, University of Hawaii, notes that the local population had advance warning of the impending eruption, leaving the island prior to its destruction. However, the thinness of the first ash layer along with the noticeable erosion of that layer by the first winter rains before the next layer was deposited, indicate that the volcano gave the local population only a few months warning.[7]
Recent archaeological 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 Dense-Rock Equivalent (DRE), or total volume of material erupted from the volcano, that was published in 1991.[8] With an estimated DRE in excess of 60 km3,[3] the volume of ejecta was up to four times what was thrown into the stratosphere by Krakatau in 1883 CE, a well-recorded event, placing the Volcanic Explosivity Index of the Thera eruption at approximately 7. The Thera volcanic events and subsequent ashfall probably sterilized the island, as occurred on Krakatau. Only the Mount Tambora volcanic eruption of 1815 CE released more material into the atmosphere during historic times.[1][2]
There were significant climatic changes during the aftermath of the eruption. Based on the observed changes to the bristlecone pines of California; the bog oaks of Ireland, England, andGermany, and the grain crops of China, it is believed that the plume from the eruption added sufficient particulates to the atmosphere to have reduced temperatures worldwide.[3][2]
Archaeologists developed the Late Bronze Age chronologies of eastern Mediterranean cultures by analyzing the origin of artifacts (for example, items from Crete, mainland Greece, Cyprus or Canaan) found in each archaeological layer.[3] If the artifact's origin can be accurately dated, then 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.[13] Archeological digs on Akrotiri have also yielded fragments of nine Syro-Palestinian Middle Bronze II (MBII) gypsum vessels.[12]
At one time, it was believed that data from Greenland ice cores and tree-ring dating, could be useful in ascertaining the exact date of the eruption. A large eruption, identified in ice cores and dated to 1644 BCE (+/- 20 years) was suspected to be Santorini. Previously, it was assumed that the ice core and tree-ring data were related. However, volcanic ash retrieved from an ice core demonstrated that this was not from Santorini, leading to the conclusion that the eruption may have occurred on another date.[9] The late Holocene eruption of the Mount Aniakchak, a volcano in Alaska, is proposed as the most likely source of the minute shards of volcanic glass in the Greenland ice core.[16]
Tree-ring data showed that a large event interfering with normal tree growth in North America occurred in 1629-1628 BCE.[17] Further evidence of an eruption of Thera around 1628 BCE was found in studies of growth depression of European oaks in Sweden.[18]
In 2006, two research papers were published arguing that new radiocarbon analysis dated the eruption between 1627 and 1600 BCE. Samples of wood, bone, and seed collected from various locations in the Aegean, including Santorini, Crete, Rhodes and Turkey, were analyzed at three separate labs in Oxford, Vienna, Austria, and Heidelberg, Germany in order to minimise the chance of a radiocarbon dating error. Results of the analysis indicated a broad dating for the Thera event between 1660 to 1613 BCE.[19]
The date of the eruption of Thera was recently narrowed to between 1627-1600 BCE, with a 95% probability of accuracy, after researchers analyzed material from an olive tree that was found buried beneath a lava flow from the volcano.[20] Because the tree grew on the island, the results may have been affected by volcanic outgassing, which would have skewed the accuracy of the radiometric studies.
Although radiocarbon dating and tree-ring analysis indicate 1600 BCE eruption dating, archeologists believe that the date is contradicted by findings in Egyptian and Theran excavations. For example, some archeologists have found buried Egyptian and Cypriot pottery on Thera that is dated to a later period than the radiometric dates for the eruption. Since the Egyptian historical chronology has been established by numerous archeological studies, the exact date of the eruption remains controversial. If radiocarbon dating is accurate, there would be significant chronological realignment of several Eastern Mediterranean cultures.[21][22]
Significant Minoan remains have been found above the Late Minoan I era Thera ash layer, implying that the Thera eruption did not cause the immediate downfall of the Minoans. The Mycenaean conquest of the Minoans occurred in Late Minoan II period, not many years after the eruption, and many archaeologists speculate that the eruption induced a crisis in Minoan civilization, which allowed the Mycenaeans to conquer them easily.[25]
Heavy 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.[3][30][31] This theory is not supported by current archaeological evidence which show no pumice layers at Avaris or elsewhere in Lower Egypt during the reigns of Ahmose I and Thutmosis III. While it has been argued that the damage from 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.[32]
There is a consensus that Egypt, being far away from areas of significant seismic activity, would not be significantly affected by an earthquake in the Aegean. Furthermore, other documents, such as Hatshepsut's Speos Armedios, depict similar storms, but are clearly speaking figuratively, not literally. Research indicates that this particular stele is just another reference to the Pharaoh overcoming the powers of chaos and darkness.[32]
More importantly though, the chronology of events as presented in Exodus drastically differs from those that would have preceded from a volcanic eruption. For example, the plague of darkness came last in Exodus. In reality, darkness caused by volcanic ash would have preceded displaced frogs, hail, or a "river of blood." These effects would only have appeared after an eruption had taken place. Further, assuming the eruption had caused any of the plagues, any sort of accompanying tsunami would have taken place months before the Israelites would arrive at the Red Sea. By that time, the waters would have recessed, blocking any sort of passage on dry land.
Santorini (Σαντορίν?
..... Click the link for more information.
The Aegean Sea (pronounced [i:ˈdʒi:ən/span>]], Greek:
..... Click the link for more information.
..... Click the link for more information.
Santorini (Σαντορίν?
..... Click the link for more information.
The eruption caused significant climatic changes in the eastern Mediterranean region, Aegean Sea and much of the Northern Hemisphere.[3] There is also evidence that the eruption caused failure of crops in China, inspired certain Greek myths, contributed to turmoil in Egypt, and influenced many of the biblical Exodus stories.[3][3][3] It is also theorized to have been the basis of the story of Atlantis.[4]
Eruption
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.[5] Another famous volcano known to repeat a similar process is Krakatoa in Indonesia.
Immediately prior to the Minoan eruption, the walls of the caldera formed a nearly continuous ring of islands with the only entrance lying between Thera and the tiny island of Aspronisi.[5] 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.
On Santorini, there is a m ( ft) thick layer of white tephra that overlies the soil clearly delineating the ground level prior to the eruption. This layer has three distinct bands that indicate the different phases of the eruption.[6] Since no bodies have been found at the Akrotiri site, Floyd W. McCoy, Professor of Geology and Oceanography, University of Hawaii, notes that the local population had advance warning of the impending eruption, leaving the island prior to its destruction. However, the thinness of the first ash layer along with the noticeable erosion of that layer by the first winter rains before the next layer was deposited, indicate that the volcano gave the local population only a few months warning.[7]
Recent archaeological 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 Dense-Rock Equivalent (DRE), or total volume of material erupted from the volcano, that was published in 1991.[8] With an estimated DRE in excess of 60 km3,[3] the volume of ejecta was up to four times what was thrown into the stratosphere by Krakatau in 1883 CE, a well-recorded event, placing the Volcanic Explosivity Index of the Thera eruption at approximately 7. The Thera volcanic events and subsequent ashfall probably sterilized the island, as occurred on Krakatau. Only the Mount Tambora volcanic eruption of 1815 CE released more material into the atmosphere during historic times.[1][2]
Physical consequences
The plinian eruption resulted in an estimated km ( mi) to km ( mi) high 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 event also generated a m ( ft) to m ( ft) high tsunami that devastated the north coast of Crete, km ( mi) away. The tsunami impacted coastal towns such as Amnisos, where building walls were knocked out of alignment. On the island of Anafi, km ( mi) to the east, ash layers m ( ft) deep have been found, as well as pumice layers on slopes m ( ft) above sea level. Elsewhere in the Mediterranean there are pumice deposits which could have been caused by the Thera eruption.[9] 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 would have had little impact on the island.[9] 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.[10][11]There were significant climatic changes during the aftermath of the eruption. Based on the observed changes to the bristlecone pines of California; the bog oaks of Ireland, England, andGermany, and the grain crops of China, it is believed that the plume from the eruption added sufficient particulates to the atmosphere to have reduced temperatures worldwide.[3][2]
Dating
The Minoan eruption provides a fixed point for aligning the entire chronology of the 2nd millennium BCE in the Aegean, because evidence of the eruption is found throughout the region. Despite this evidence, the exact date of the eruption has been difficult to determine. Current estimates based on radiocarbon dating indicate that the eruption occurred between 1630 and 1600 BCE.[12] However, this range of dates conflicts with the previous estimate of approximately 1550 BCE based on archaeological studies utilizing Conventional Egyptian chronology.[3]Archaeologists developed the Late Bronze Age chronologies of eastern Mediterranean cultures by analyzing the origin of artifacts (for example, items from Crete, mainland Greece, Cyprus or Canaan) found in each archaeological layer.[3] If the artifact's origin can be accurately dated, then 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.[13] Archeological digs on Akrotiri have also yielded fragments of nine Syro-Palestinian Middle Bronze II (MBII) gypsum vessels.[12]
At one time, it was believed that data from Greenland ice cores and tree-ring dating, could be useful in ascertaining the exact date of the eruption. A large eruption, identified in ice cores and dated to 1644 BCE (+/- 20 years) was suspected to be Santorini. Previously, it was assumed that the ice core and tree-ring data were related. However, volcanic ash retrieved from an ice core demonstrated that this was not from Santorini, leading to the conclusion that the eruption may have occurred on another date.[9] The late Holocene eruption of the Mount Aniakchak, a volcano in Alaska, is proposed as the most likely source of the minute shards of volcanic glass in the Greenland ice core.[16]
Tree-ring data showed that a large event interfering with normal tree growth in North America occurred in 1629-1628 BCE.[17] Further evidence of an eruption of Thera around 1628 BCE was found in studies of growth depression of European oaks in Sweden.[18]
In 2006, two research papers were published arguing that new radiocarbon analysis dated the eruption between 1627 and 1600 BCE. Samples of wood, bone, and seed collected from various locations in the Aegean, including Santorini, Crete, Rhodes and Turkey, were analyzed at three separate labs in Oxford, Vienna, Austria, and Heidelberg, Germany in order to minimise the chance of a radiocarbon dating error. Results of the analysis indicated a broad dating for the Thera event between 1660 to 1613 BCE.[19]
The date of the eruption of Thera was recently narrowed to between 1627-1600 BCE, with a 95% probability of accuracy, after researchers analyzed material from an olive tree that was found buried beneath a lava flow from the volcano.[20] Because the tree grew on the island, the results may have been affected by volcanic outgassing, which would have skewed the accuracy of the radiometric studies.
Although radiocarbon dating and tree-ring analysis indicate 1600 BCE eruption dating, archeologists believe that the date is contradicted by findings in Egyptian and Theran excavations. For example, some archeologists have found buried Egyptian and Cypriot pottery on Thera that is dated to a later period than the radiometric dates for the eruption. Since the Egyptian historical chronology has been established by numerous archeological studies, the exact date of the eruption remains controversial. If radiocarbon dating is accurate, there would be significant chronological realignment of several Eastern Mediterranean cultures.[21][22]
Historical impact
Minoan civilization
According to several researchers, tsunamis caused by pyroclastic flows and caldera collapse destroyed the navy, merchant vessels and ports of the Minoans on the north side of Crete. As the Minoans were a sea power and depended on their naval and merchant ships for their livelihood, the Thera eruption caused significant economic hardship to the Minoans. Whether these effects were enough to trigger the downfall of the Minoans is under intense debate. Early research into the effect on the Minoans concluded that the ashfall from Thera on the eastern half of Crete choked off plant life, causing starvation of the local population. It was originally thought that cm ( in) to cm ( in) of ash fell on Kato Zakro, while cm ( in) fell on Knossos. However, after more thorough field examinations, this theory has lost credibility, as it has been determined that no more than mm ( in) of ash fell anywhere on Crete.[23][9][3][24][25][26]Significant Minoan remains have been found above the Late Minoan I era Thera ash layer, implying that the Thera eruption did not cause the immediate downfall of the Minoans. The Mycenaean conquest of the Minoans occurred in Late Minoan II period, not many years after the eruption, and many archaeologists speculate that the eruption induced a crisis in Minoan civilization, which allowed the Mycenaeans to conquer them easily.[25]
Chinese records
Some scientists correlate a volcanic winter from the Minoan eruption with Chinese records documenting the collapse of the 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".[3][3]Impact on Egyptian history
There are no surviving Egyptian records of the eruption, and the absence of such records is sometimes attributed to the general disorder in Egypt around the Second Intermediate Period. However, there are connections between the Thera eruption and the calamities of the Admonitions of Ipuwer, a text from Lower Egypt during the Middle Kingdom or Second Intermediate Period.[28]Heavy 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.[3][30][31] This theory is not supported by current archaeological evidence which show no pumice layers at Avaris or elsewhere in Lower Egypt during the reigns of Ahmose I and Thutmosis III. While it has been argued that the damage from 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.[32]
There is a consensus that Egypt, being far away from areas of significant seismic activity, would not be significantly affected by an earthquake in the Aegean. Furthermore, other documents, such as Hatshepsut's Speos Armedios, depict similar storms, but are clearly speaking figuratively, not literally. Research indicates that this particular stele is just another reference to the Pharaoh overcoming the powers of chaos and darkness.[32]
Greek traditions
The eruption of Thera and volcanic fallout inspired myths of the Titanomachy in Hesiod's Theogony. The background of the Titanomachy is known to derive from the Kumarbi cycle, a Bronze Age Hurrian epic from the Lake Van region. However, the Titanomachy itself 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' 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.[33]Biblical traditions
Some researchers have claimed that some of the ten plagues resulted from the eruption of Thera; however, the presumed dates of the events of Exodus, approximately 1450 BCE is almost 150 years after the radiometric date of the eruption.[34] According to the Bible, Egypt was beset by such misfortunes as the transforming of their water supply to blood, the infestations of frogs, gnats, and flies, darkness, and violent hail. These effects are compatible with the catastrophic eruption of a volcano in different ways. While the "blood" in the water could have been red tide which is poisonous to human beings, the frogs may have been displaced by the eruption, and their eventual death would have given rise to large numbers of scavenging insects. The darkness could have been the resulting volcanic winter, and the hail the large chunks of ejecta spewn from the volcano. The tsunami that resulted from the Thera eruption could have been the basis for the myth of the parting of the sea, when the sea receded from the shore immediately prior to the arrival of the tsunami. Shallow areas of the sea would have allowed the Israelites, under Moses, safe passage across the Red Sea, while the ensuing tsunami devastated the Egyptian army. Exodus mentions that the Israelites were guided by a "pillar of smoke" during the day and a "pillar of fire" at night, which many scholars have speculated that it refers to volcanic activity. However, unambiguous radiometric dating of Thera eruption places it at a date significantly different from the proposed dates of the Exodus from Egypt.[35][36][3]More importantly though, the chronology of events as presented in Exodus drastically differs from those that would have preceded from a volcanic eruption. For example, the plague of darkness came last in Exodus. In reality, darkness caused by volcanic ash would have preceded displaced frogs, hail, or a "river of blood." These effects would only have appeared after an eruption had taken place. Further, assuming the eruption had caused any of the plagues, any sort of accompanying tsunami would have taken place months before the Israelites would arrive at the Red Sea. By that time, the waters would have recessed, blocking any sort of passage on dry land.
References
1. ^ Oppenheimer, Clive (2003). "Climatic, environmental and human consequences of the largest known historic eruption: Tambora volcano (Indonesia) 1815". Progress in Physical Geography 27 (2): 230-259.
2. ^ McCoy, FW, & Dunn, SE (2002). "Modelling the Climatic Effects of the LBA Eruption of Thera: New Calculations of Tephra Volumes May Suggest a Significantly Larger Eruption than Previously Reported". Chapman Conference on Volcanism and the Earth's Atmosphere, Thera, Greece: American Geographical Union. Retrieved on 2007-05-29.
3. ^ Sigurdsson H, Carey, S, Alexandri M, Vougioukalakis G, Croff K, Roman C, Sakellariou D, Anagnostou C, Rousakis G, Ioakim C, Gogou A, Ballas D, Misaridis T, & Nomikou P (2006). "Marine Investigations of Greece's Santorini Volcanic Field". Eos 87 (34): 337-348.
4. ^ The wave that destroyed Atlantis Harvey Lilley, BBC News Online, 2007-04-20. Retrieved 2007-04-21.
5. ^ Friedrich, WL (1999). Fire in the Sea, the Santorini Volcano: Natural History and the Legend of Atlantis. Cambridge University Press. ISBN 0-521-65290-1.
6. ^ Davidson, DA (1979). "Aegean Soils During the Second Millennium BCE with Reference to Thera". Thera and the Aegean World I. Papers presented at the Second International Scientific Congress, Santorini, Greece, August 1978: 725-739, UK: The Thera Foundation. Retrieved on 2007-03-10.
7. ^ G, Heiken; McCoy, F (1990). "Precursory Activity to the Minoan Eruption, Thera, Greece". Thera and the Aegean World III, Vol 2: 79-88, London: The Thera Foundation.
8. ^ Santorini eruption much larger than originally believed (2006). Retrieved on 2007-03-10.
9. ^ Pumice on south Mediterranean - remnant of the Thera eruption? (2004). Retrieved on 2007-03-10.
10. ^ Stanley, DJ & Sheng, H (1986). "Volcanic shards from Santorini (Upper Minoan ash) in the Nile Delta, Egypt". Nature 320, 1986: 733-735. DOI:10.1038/320733a0.
11. ^ Guichard, F et al. (1993). "Tephra from the Minoan eruption of Santorini in sediments of the Black Sea". Nature 363 (6430): 610-612. DOI:10.1038/363610a0.
12. ^ New research in Science: date of the largest volcanic eruption in the Bronze Age finally pinpointed (2006). Retrieved on 2007-03-10.
13. ^ Lolos, YG (1989). On the Late Helladic I of Akrotiri, Thera On the Late Helladic I of Akrotiri, Thera. The Thera Foundation. Retrieved on 2007-03-10.
14. ^ Warren, PM (1989). Summary of Evidence for the Absolute Chronology of the Early Part of the Aegean Late Bronze Age Derived from Historical Egyptian Sources in: Thera and the Aegean World III, Hardy, DA (ed). The Thera Foundation, 24-26. ISBN 0 9506133 6 3. Retrieved on 2007-03-10.
15. ^ Keenan, Douglas J. (2003). "Volcanic ash retrieved from the GRIP ice core is not from Thera". Geochemistry Geophysics Geosystems 4 (11): 1097. DOI:10.1029/2003GC000608. 1525-2027. Retrieved on 2007-03-10.
16. ^ Pearce, N. J. G., J. A. Westgate, S. J. Preece, W. J. Eastwood, and W. T. Perkins (2004). "Identification of Aniakchak (Alaska) tephra in Greenland ice core challenges the 1645 BC date for Minoan eruption of Santorini". Geochem. Geophys. Geosyst. 5. DOI:10.1029/2003GC000672.
17. ^ Baillie, MGL (1989). Irish Tree Rings and an Event in 1628 BC. The Thera Foundation. Retrieved on 2007-03-10.
18. ^ Grudd, H, Briffa, KR, Gunnarson, BE, & Linderholm, HW (2000). "Swedish tree rings provide new evidence in support of a major, widespread environmental disruption in 1628 BC". Geophysical Research Letters 27 (18): 2957-2960. DOI:10.1029/1999GL010852.
19. ^ Manning, Sturt W; Ramsey, CB, Kutschera, W, Higham, T, Kromer, B, Steier, P, and Wild, EM (2006). "Chronology for the Aegean Late Bronze Age 1700-1400 B.C.". Science 312 (5773): 565-569. DOI:10.1126/science.1125682. Retrieved on 2007-03-10.
20. ^ Friedrich, Walter L; Kromer, B, Friedrich, M, Heinemeier, J, Pfeiffer, T, and Talamo, S (2006). "Santorini Eruption Radiocarbon Dated to 1627-1600 B.C.". Science 312 (5773): 548. DOI:10.1126/science.1125087. Retrieved on 2007-03-10.
21. ^ Balter, M (2006). "New Carbon Dates Support Revised History of Ancient Mediterranean". Science 312 (5773): 508-509. DOI:10.1126/science.312.5773.508. Retrieved on 2007-05-01.
22. ^ Wilford, JN. "Ancient Crete more ancient than thought? New volcanic evidence suggests discrepancy of more than a full century", The Columbus Dispatch, 2006-05-09. Retrieved on 2007-05-20.
23. ^ Callender, G (1999). The Minoans and the Mycenaeans: Aegean Society in the Bronze Age. Oxford University Press. ISBN 0195510283.
24. ^ Marinatos, S (1939). "The Volcanic Destruction of Minoan Crete". Antiquity 13: 425-439.
25. ^ Antonopoulos, J. (1992). "The great Minoan eruption of Thera volcano and the ensuing tsunami in the Greek Archipelago". Natural Hazards 5: 153-168. DOI:10.1007/BF00127003.
26. ^ Pareschi, MT, Favalli, M & Boschi, E (2006). "Impact of the Minoan tsunami of Santorini: Simulated scenarios in the eastern Mediterranean". Geophysical Research Letters 33. DOI:10.1029/2006GL027205. .
27. ^ Foster, KP, Ritner, RK, and Foster, BR (1996). "Texts, Storms, and the Thera Eruption". Journal of Near Eastern Studies 55 (1): 1-14.
28. ^ Galanopoulos, Angelos Georgiou (1969). Atlantis: The Truth Behind the Legend. Bobbs-Merrill Co. ISBN 978-0672506109.
29. ^ EN, Davis (1990). A Storm in Egypt during the Reign of Ahmose. Thera and the Aegean World III. Thera Foundation. Retrieved on 2007-03-10.
30. ^ Goedicke, Hans (1995). 'Studies about Kamose and Ahmose'. Baltimore: David Brown Book Company, Chapter 3. ISBN 0-9613805-8-6.
31. ^ Foster, KP & Ritner, RK (1996). "Texts, Storms, and the Theran Eruption". Journal of Near Eastern Studies 57: 1-14.
32. ^ Wiener, MH; Allen, JP (1998). "Separate Lives: The Ahmose Tempest Stela and the Theran Eruption". Journal of Near Eastern Studies 57: 1-28.
33. ^ Luce, John Victor (1969). The end of Atlantis: New light on an old legend (New Aspects of Antiquity). London: Thames & Hudson. ISBN 978-0500390054.
34. ^ Bennett, JG (1963). "Geo-Physics and Human History: New Light on Plato's Atlantis and the Exodus". Systematics 1 (2). Retrieved on 2007-05-22.
35. ^ Phillips, G (2003). Atlantis and the Ten Plagues of Egypt: The Secret History Hidden in the Valley of the Kings. Bear & Company. ISBN 978-1591430094.
36. ^ Phillips, G. Act of God. Graham Phillips. Retrieved on 2007-05-22.
37. ^ LaMoreaux, PE (1995). "Worldwide environmental impacts from the eruption of Thera". Environmental Geology 26 (3): 172-181. DOI:10.1007/BF00768739.
2. ^ McCoy, FW, & Dunn, SE (2002). "Modelling the Climatic Effects of the LBA Eruption of Thera: New Calculations of Tephra Volumes May Suggest a Significantly Larger Eruption than Previously Reported". Chapman Conference on Volcanism and the Earth's Atmosphere, Thera, Greece: American Geographical Union. Retrieved on 2007-05-29.
3. ^ Sigurdsson H, Carey, S, Alexandri M, Vougioukalakis G, Croff K, Roman C, Sakellariou D, Anagnostou C, Rousakis G, Ioakim C, Gogou A, Ballas D, Misaridis T, & Nomikou P (2006). "Marine Investigations of Greece's Santorini Volcanic Field". Eos 87 (34): 337-348.
4. ^ The wave that destroyed Atlantis Harvey Lilley, BBC News Online, 2007-04-20. Retrieved 2007-04-21.
5. ^ Friedrich, WL (1999). Fire in the Sea, the Santorini Volcano: Natural History and the Legend of Atlantis. Cambridge University Press. ISBN 0-521-65290-1.
6. ^ Davidson, DA (1979). "Aegean Soils During the Second Millennium BCE with Reference to Thera". Thera and the Aegean World I. Papers presented at the Second International Scientific Congress, Santorini, Greece, August 1978: 725-739, UK: The Thera Foundation. Retrieved on 2007-03-10.
7. ^ G, Heiken; McCoy, F (1990). "Precursory Activity to the Minoan Eruption, Thera, Greece". Thera and the Aegean World III, Vol 2: 79-88, London: The Thera Foundation.
8. ^ Santorini eruption much larger than originally believed (2006). Retrieved on 2007-03-10.
9. ^ Pumice on south Mediterranean - remnant of the Thera eruption? (2004). Retrieved on 2007-03-10.
10. ^ Stanley, DJ & Sheng, H (1986). "Volcanic shards from Santorini (Upper Minoan ash) in the Nile Delta, Egypt". Nature 320, 1986: 733-735. DOI:10.1038/320733a0.
11. ^ Guichard, F et al. (1993). "Tephra from the Minoan eruption of Santorini in sediments of the Black Sea". Nature 363 (6430): 610-612. DOI:10.1038/363610a0.
12. ^ New research in Science: date of the largest volcanic eruption in the Bronze Age finally pinpointed (2006). Retrieved on 2007-03-10.
13. ^ Lolos, YG (1989). On the Late Helladic I of Akrotiri, Thera On the Late Helladic I of Akrotiri, Thera. The Thera Foundation. Retrieved on 2007-03-10.
14. ^ Warren, PM (1989). Summary of Evidence for the Absolute Chronology of the Early Part of the Aegean Late Bronze Age Derived from Historical Egyptian Sources in: Thera and the Aegean World III, Hardy, DA (ed). The Thera Foundation, 24-26. ISBN 0 9506133 6 3. Retrieved on 2007-03-10.
15. ^ Keenan, Douglas J. (2003). "Volcanic ash retrieved from the GRIP ice core is not from Thera". Geochemistry Geophysics Geosystems 4 (11): 1097. DOI:10.1029/2003GC000608. 1525-2027. Retrieved on 2007-03-10.
16. ^ Pearce, N. J. G., J. A. Westgate, S. J. Preece, W. J. Eastwood, and W. T. Perkins (2004). "Identification of Aniakchak (Alaska) tephra in Greenland ice core challenges the 1645 BC date for Minoan eruption of Santorini". Geochem. Geophys. Geosyst. 5. DOI:10.1029/2003GC000672.
17. ^ Baillie, MGL (1989). Irish Tree Rings and an Event in 1628 BC. The Thera Foundation. Retrieved on 2007-03-10.
18. ^ Grudd, H, Briffa, KR, Gunnarson, BE, & Linderholm, HW (2000). "Swedish tree rings provide new evidence in support of a major, widespread environmental disruption in 1628 BC". Geophysical Research Letters 27 (18): 2957-2960. DOI:10.1029/1999GL010852.
19. ^ Manning, Sturt W; Ramsey, CB, Kutschera, W, Higham, T, Kromer, B, Steier, P, and Wild, EM (2006). "Chronology for the Aegean Late Bronze Age 1700-1400 B.C.". Science 312 (5773): 565-569. DOI:10.1126/science.1125682. Retrieved on 2007-03-10.
20. ^ Friedrich, Walter L; Kromer, B, Friedrich, M, Heinemeier, J, Pfeiffer, T, and Talamo, S (2006). "Santorini Eruption Radiocarbon Dated to 1627-1600 B.C.". Science 312 (5773): 548. DOI:10.1126/science.1125087. Retrieved on 2007-03-10.
21. ^ Balter, M (2006). "New Carbon Dates Support Revised History of Ancient Mediterranean". Science 312 (5773): 508-509. DOI:10.1126/science.312.5773.508. Retrieved on 2007-05-01.
22. ^ Wilford, JN. "Ancient Crete more ancient than thought? New volcanic evidence suggests discrepancy of more than a full century", The Columbus Dispatch, 2006-05-09. Retrieved on 2007-05-20.
23. ^ Callender, G (1999). The Minoans and the Mycenaeans: Aegean Society in the Bronze Age. Oxford University Press. ISBN 0195510283.
24. ^ Marinatos, S (1939). "The Volcanic Destruction of Minoan Crete". Antiquity 13: 425-439.
25. ^ Antonopoulos, J. (1992). "The great Minoan eruption of Thera volcano and the ensuing tsunami in the Greek Archipelago". Natural Hazards 5: 153-168. DOI:10.1007/BF00127003.
26. ^ Pareschi, MT, Favalli, M & Boschi, E (2006). "Impact of the Minoan tsunami of Santorini: Simulated scenarios in the eastern Mediterranean". Geophysical Research Letters 33. DOI:10.1029/2006GL027205. .
27. ^ Foster, KP, Ritner, RK, and Foster, BR (1996). "Texts, Storms, and the Thera Eruption". Journal of Near Eastern Studies 55 (1): 1-14.
28. ^ Galanopoulos, Angelos Georgiou (1969). Atlantis: The Truth Behind the Legend. Bobbs-Merrill Co. ISBN 978-0672506109.
29. ^ EN, Davis (1990). A Storm in Egypt during the Reign of Ahmose. Thera and the Aegean World III. Thera Foundation. Retrieved on 2007-03-10.
30. ^ Goedicke, Hans (1995). 'Studies about Kamose and Ahmose'. Baltimore: David Brown Book Company, Chapter 3. ISBN 0-9613805-8-6.
31. ^ Foster, KP & Ritner, RK (1996). "Texts, Storms, and the Theran Eruption". Journal of Near Eastern Studies 57: 1-14.
32. ^ Wiener, MH; Allen, JP (1998). "Separate Lives: The Ahmose Tempest Stela and the Theran Eruption". Journal of Near Eastern Studies 57: 1-28.
33. ^ Luce, John Victor (1969). The end of Atlantis: New light on an old legend (New Aspects of Antiquity). London: Thames & Hudson. ISBN 978-0500390054.
34. ^ Bennett, JG (1963). "Geo-Physics and Human History: New Light on Plato's Atlantis and the Exodus". Systematics 1 (2). Retrieved on 2007-05-22.
35. ^ Phillips, G (2003). Atlantis and the Ten Plagues of Egypt: The Secret History Hidden in the Valley of the Kings. Bear & Company. ISBN 978-1591430094.
36. ^ Phillips, G. Act of God. Graham Phillips. Retrieved on 2007-05-22.
37. ^ LaMoreaux, PE (1995). "Worldwide environmental impacts from the eruption of Thera". Environmental Geology 26 (3): 172-181. DOI:10.1007/BF00768739.
Bibliography
- Callender, G (1999). The Minoans and the Mycenaeans: Aegean Society in the Bronze Age. Oxford University Press. ISBN 0195510283.
- Forsyth, PY (1997). Thera in the Bronze Age. Peter Lang Publishing. ISBN 0-8204-4889-3.
- Friedrich, WL (1999). Fire in the Sea, the Santorini Volcano: Natural History and the Legend of Atlantis. Cambridge University Press. ISBN 0-521-65290-1.
- Greene, MT (2000). Natural Knowledge in Preclassical Antiquity. Johns Hopkins University Press. ISBN 978-0801863714.
- Phillips, G (2003). Atlantis and the Ten Plagues of Egypt: The Secret History Hidden in the Valley of the Kings. Bear & Company. ISBN 978-1591430094.
External links
- 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.
- Date of the largest volcanic eruption in the Bronze Age finally pinpointed Ã…rhus University press release about the olive tree of Friedrich et al. (scientific article but also reader friendly)
- 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
- Thera redirects here. For the moth genus, see Thera (moth). See also Dorsum Thera, a wrinkle ridge on the Moon.
Santorini (Σαντορίν?
..... Click the link for more information.
The Volcanic Explosivity Index (VEI) was devised by Chris Newhall of the U.S. Geological Survey and Steve Self at the University of Hawaii in 1982 to provide a relative measure of the explosiveness of volcanic eruptions.
..... Click the link for more information.
..... Click the link for more information.
106 (E9): 20621–20628. Retrieved on 2007-04-15.
..... Click the link for more information.
..... Click the link for more information.
Catastrophe, from the Greek Καταστροφή (katastrephein), literally means "to turn" (strephein) "downwards" (kata-).
..... Click the link for more information.
..... Click the link for more information.
Volcano:
1. Large magma chamber
2. Bedrock
3. Conduit (pipe)
4. Base
5. Sill
6. Branch pipe
7. Layers of ash emitted by the volcano
8. Flank 9. Layers of lava emitted by the volcano
10. Throat
11. Parasitic cone
12. Lava flow
13. Vent
14.
..... Click the link for more information.
1. Large magma chamber
2. Bedrock
3. Conduit (pipe)
4. Base
5. Sill
6. Branch pipe
7. Layers of ash emitted by the volcano
8. Flank 9. Layers of lava emitted by the volcano
10. Throat
11. Parasitic cone
12. Lava flow
13. Vent
14.
..... Click the link for more information.
History is the study of the past, focused on human activity and leading up to the present day.[1] More precisely, history is the continuous, systematic narrative and research of past events as relating to the human race [1]
..... Click the link for more information.
..... Click the link for more information.
Crete (Greek Κρήτη—classical transliteration Krētē, modern Greek transliteration KrÃti; Ottoman Turkish گريد (Girit); Classical Latin Crēta, Vulgar Latin Candia
..... Click the link for more information.
..... Click the link for more information.
The Minoan civilization was a bronze age civilization which arose on Crete, an island in the Aegean Sea. The Minoan culture flourished from approximately 2700 to 1450 BC; afterwards, Mycenaean Greek culture became dominant on Crete.
..... Click the link for more information.
..... Click the link for more information.
Mediterranean is a sea of the Atlantic Ocean almost completely enclosed by land: on the north by Europe, on the south by Africa, and on the east by Asia. It covers an approximate area of 2.
..... Click the link for more information.
..... Click the link for more information.
For the ship Aegean Sea, see .
The Aegean Sea (pronounced [i:ˈdʒi:ən/span>]], Greek:
..... Click the link for more information.
Northern Hemisphere or northern hemisphere[1] is the half of a planet that is north of the equator—the word hemisphere literally means 'half ball'. It is also that half of the celestial sphere north of the celestial equator.
..... Click the link for more information.
..... Click the link for more information.
This page contains Chinese text.
Without proper rendering support, you may see question marks, boxes, or other symbols instead of Chinese characters.
China (Traditional Chinese: Without proper rendering support, you may see question marks, boxes, or other symbols instead of Chinese characters.
..... Click the link for more information.
Greek mythology is the body of stories belonging to the Ancient Greeks concerning their gods and heroes, the nature of the world and the origins and significance of their own cult and ritual practices.
..... Click the link for more information.
..... Click the link for more information.
Gumhūriyyat Miṣr al-ʿArabiyyah
Flag Coat of arms
Anthem
Bilady, Bilady, Bilady
..... Click the link for more information.
Arab Republic of Egypt
Flag Coat of arms
Anthem
Bilady, Bilady, Bilady
..... Click the link for more information.
The Bible is
Bible
..... Click the link for more information.
- Part of
- (see The Hebrew Bible below)
- Part of a series on Christianity
- (see The New Testament below)
Bible
..... Click the link for more information.
Tanakh
Torah | Nevi'im | Ketuvim
Books of the Torah
1. Genesis
2. Exodus
3. Leviticus
4. Numbers
5.
..... Click the link for more information.
Torah | Nevi'im | Ketuvim
Books of the Torah
1. Genesis
2. Exodus
3. Leviticus
4. Numbers
5.
..... Click the link for more information.
Atlantis (in Greek, Ἀτλαντὶς νῆσος, "island of Atlas") is the name of a legendary island first mentioned in Plato's dialogues Timaeus and Critias.
..... Click the link for more information.
..... Click the link for more information.
caldera is a volcanic feature formed by the collapse of land following a volcanic eruption. They are often confused with volcanic craters. The word 'caldera' comes from the Spanish language, meaning "cauldron".
..... Click the link for more information.
..... Click the link for more information.
KRAKATOA is a modular explosive device used for explosive ordnance disposal (EOD) or demolitions. It was developed by the British company Alford Technologies and has been featured during the second season of Discovery Channel's Future Weapons television series.
..... Click the link for more information.
..... Click the link for more information.
Motto
"Bhinneka Tunggal Ika" (Old Javanese)
"Unity in Diversity"
National ideology: Pancasila[1]
Anthem
Indonesia Raya
..... Click the link for more information.
"Bhinneka Tunggal Ika" (Old Javanese)
"Unity in Diversity"
National ideology: Pancasila[1]
Anthem
Indonesia Raya
..... Click the link for more information.
Nea Kameni is a small uninhabited Greek island of volcanic origin located in the Bay of Santorini. It was first formed in 16th century through volcanic eruptions, and was enlarged the same way. The last (small) eruption happened in 1950.
..... Click the link for more information.
..... Click the link for more information.
- Thera redirects here. For the moth genus, see Thera (moth). See also Dorsum Thera, a wrinkle ridge on the Moon.
Santorini (Σαντορίν?
..... Click the link for more information.
Tephra is air-fall material produced by a volcanic eruption regardless of composition or fragment size. Tephra is typically rhyolitic in composition as most explosive volcanoes are the product of the more viscous felsic or high silica magmas.
..... Click the link for more information.
..... Click the link for more information.
University of Hawaiʻi, formally the University of Hawaiʻi System and popularly known as UH
..... Click the link for more information.
..... Click the link for more information.
106 (E9): 20621–20628. Retrieved on 2007-04-15.
..... Click the link for more information.
..... Click the link for more information.
In volcanology, ejecta consists of particles that came out of a volcanic vent, traveled through the air or under water, and fell back on the ground surface or on the ocean floor.
..... Click the link for more information.
..... Click the link for more information.
KRAKATOA is a modular explosive device used for explosive ordnance disposal (EOD) or demolitions. It was developed by the British company Alford Technologies and has been featured during the second season of Discovery Channel's Future Weapons television series.
..... Click the link for more information.
..... Click the link for more information.
18th century - 19th century - 20th century
1850s 1860s 1870s - 1880s - 1890s 1900s 1910s
1880 1881 1882 - 1883 - 1884 1885 1886
:
Subjects: Archaeology - Architecture -
..... Click the link for more information.
1850s 1860s 1870s - 1880s - 1890s 1900s 1910s
1880 1881 1882 - 1883 - 1884 1885 1886
:
Subjects: Archaeology - Architecture -
..... Click the link for more information.
The Volcanic Explosivity Index (VEI) was devised by Chris Newhall of the U.S. Geological Survey and Steve Self at the University of Hawaii in 1982 to provide a relative measure of the explosiveness of volcanic eruptions.
..... Click the link for more information.
..... Click the link for more information.
Mount Tambora (or Tomboro) is an active stratovolcano on Sumbawa island, Indonesia. Sumbawa is flanked both to the north and south by oceanic crust, and Tambora was formed by the active subduction zones beneath it.
..... Click the link for more information.
..... Click the link for more information.
This article is copied from an article on Wikipedia.org - the free encyclopedia created and edited by online user community. The text was not checked or edited by anyone on our staff. Although the vast majority of the wikipedia encyclopedia articles provide accurate and timely information please do not assume the accuracy of any particular article. This article is distributed under the terms of GNU Free Documentation License.
Herod_Archelaus
