Santorini caldera: Difference between revisions
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==Geology== |
==Geology== |
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[[File:Southern aegean volcanic arc.jpg|thumb|right|The [[South Aegean Volcanic Arc]] includes the volcanoes of Methana, Milos, Santorini and Nisyros.]] |
[[File:Southern aegean volcanic arc.jpg|thumb|right|The [[South Aegean Volcanic Arc]] includes the volcanoes of Methana, Milos, Santorini and Nisyros.]] |
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The volcanic complex of Santorini is the most active part of the [[South Aegean Volcanic Arc]], which includes the volcanoes of [[Methana]], [[Milos]], Santorini and [[Nisyros]]. It is formed by the subduction of the African [[tectonic plate]] underneath the Aegean subplate of the Eurasian tectonic plate, which occurs at a rate of up to 5 cm per year in a northeasterly direction. This subduction causes earthquakes at depths of 150–170 km.<ref name="Pfeiffer2">{{cite web|url=http://www.decadevolcano.net/santorini/santorini_geology_geography.htm |title=Tectonic setting of Santorini |accessdate=2011-04-20}}</ref> |
The volcanic complex of Santorini is the most active part of the [[South Aegean Volcanic Arc]], which includes the volcanoes of [[Methana]] on the mainland of Greece, [[Milos]], Santorini and [[Nisyros]]. It is formed by the subduction of the African [[tectonic plate]] underneath the Aegean subplate of the Eurasian tectonic plate, which occurs at a rate of up to 5 cm per year in a northeasterly direction. This subduction causes earthquakes at depths of 150–170 km.<ref name="Pfeiffer2">{{cite web|url=http://www.decadevolcano.net/santorini/santorini_geology_geography.htm |title=Tectonic setting of Santorini |accessdate=2011-04-20}}</ref> |
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Non-volcanic rocks are exposed on Santorini at [[Mikro Profititis Ilias]], Mesa Vouno, the Gavrillos ridge, Pirgos, Monolithos and the inner side of the caldera wall between Cape Plaka and Athinios.<ref name="Pfeiffer3">{{cite web |url=http://www.decadevolcano.net/santorini/santorini_geohist.htm#basement |title=Geology of Santorini – The prevolcanic basement |accessdate=2011-04-20}}</ref> |
Non-volcanic rocks are exposed on Santorini at [[Mikro Profititis Ilias]], Mesa Vouno, the Gavrillos ridge, Pirgos, Monolithos and the inner side of the caldera wall between Cape Plaka and Athinios.<ref name="Pfeiffer3">{{cite web |url=http://www.decadevolcano.net/santorini/santorini_geohist.htm#basement |title=Geology of Santorini – The prevolcanic basement |accessdate=2011-04-20}}</ref> |
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Revision as of 17:41, 1 April 2022
| Santorini Caldera | |
|---|---|
 Santorini island group from space | |
| Highest point | |
| Coordinates | 36°23′44″N 25°27′33″E / 36.39556°N 25.45917°E |
| Geography | |
 | |
| Location | Aegean Sea, Greece |
| Geology | |
| Mountain type | Caldera (active) |
| Last eruption | January to February 1950 |
Santorini caldera is a large, mostly submerged caldera, located in the southern Aegean Sea, 120 kilometers north of Crete in Greece. Visible above water is the circular Santorini island group, consisting of Santorini (classic Greek Thera), the main island, Therasia and Aspronisi at the periphery, and the Kameni islands at the center. It has been designated a Decade Volcano.
Geography
The caldera measures about 12 by 7 km (7.5 by 4.3 mi), with 300 m (980 ft) high steep cliffs on three sides.
There are two small volcanic islands at the center of the caldera, Nea ("New") Kameni and Palea ("Old") Kameni.
The main island, Santorini has an area of 75.8 km2 (29.3 sq mi), Therasia 9.3 km2 (3.6 sq mi), and the uninhabited islands of Nea Kameni 3.4 km2 (1.3 sq mi), Palea Kameni 0.5 km2 (0.19 sq mi) and Aspronisi 0.1 km2 (0.039 sq mi).
Santorini's high walls, draped by whitewashed villages, combined with a sunny climate and good observation conditions, have made it a magnet for volcanologists,[1] as well as a highlight of tourism in the Aegean.
Geology
The volcanic complex of Santorini is the most active part of the South Aegean Volcanic Arc, which includes the volcanoes of Methana on the mainland of Greece, Milos, Santorini and Nisyros. It is formed by the subduction of the African tectonic plate underneath the Aegean subplate of the Eurasian tectonic plate, which occurs at a rate of up to 5 cm per year in a northeasterly direction. This subduction causes earthquakes at depths of 150–170 km.[2]
Non-volcanic rocks are exposed on Santorini at Mikro Profititis Ilias, Mesa Vouno, the Gavrillos ridge, Pirgos, Monolithos and the inner side of the caldera wall between Cape Plaka and Athinios.[3]
The Kameni islands at the center of the caldera are made of lava rocks.
Volcanology
The caldera of Santorini lies in the center of the Christiana-Santorini-Kolumbo volcanic field, which comprises the extinct Christiana Volcano, the Santorini Caldera, the polygenetic submarine Kolumbo Volcano, as well as the Kolumbo Volcanic Chain. [4] This volcanic lineament evolved during four main phases of volcanic activity, which initiated in the Pliocene from several local centers that only recently matured to form the vast Santorini edifice. The present-day caldera is composed of overlapping shield volcanoes, cut by at least four partially overlapping calderas, of which the oldest southern caldera was formed about 180,000 years before the present era (BP). The subsequent Skaros caldera was created about 70,000 years BP, and the Cape Riva caldera about 21,000 years BP. The current caldera was formed about 3600 years BP during the Minoan eruption.[5]
Palea Kameni and Nea Kameni were formed as a result of multiple, initially submarine, smaller eruptions at the center of the caldera.[6]
Although dormant, Santorini is an active volcano. Numerous minor and medium-sized, mainly effusive, eruptions have built the dark-colored lava shields of Nea and Palea Kameni inside the caldera.
Their last eruption was in 1950, and now only fumarolic activity, primarily inside the recently active craters, takes place.[1] GPS instruments registered renewed deformation around the caldera in 2011 and 2012.[7]
The huge Minoan eruption of Santorini in the 17th century BC may have inspired the legend of Atlantis.[8] It was rated 7, the highest score for a historical eruption, in the Smithsonian Global Volcanism Program's Volcanic Explosivity Index.[9]
Eruptive history
Following is a list of the major eruptive events of Santorini beginning with the catastrophic Minoan eruption, as noted by the Smithsonian National Museum of Natural History's Global Volcanism Program:[5]
| Start date | Stop date | Characteristics of eruption |
|---|---|---|
| 1610 BC ± 14 years ("Minoan eruption") |
Unknown | Central vent eruption, regional fissure eruption, submarine eruption, explosive eruption, pyroclastic flows and pyroclastic surges, phreatic explosions, extensive physical damage, massive lava fountains and extensive lava flows, minor mudflows on the sea, megatsunamis, caldera collapse, fatalities, mass evacuation. |
| 197 BC | Unknown | Central vent eruption, regional fissure eruption, submarine eruption, new island formation, explosive eruption. |
| Dec 31, 46 AD | Feb 1, 47 AD ± 30 days | Central vent eruption, regional fissure eruption, submarine eruption, new island formation, explosive eruption, lava flows, lava dome extrusion, tsunami. |
| Jul 15 726 AD ± 45 days | Unknown | Central vent eruption, regional fissure eruption, submarine eruption, new island formation, explosive eruption, lava flows, lava dome extrusion, damage. |
| 1570 | 1573 | Central vent eruption, regional fissure eruption, submarine eruption, new island formation, explosive eruption, lava flows, lava dome extrusion. |
| Sep. 27, 1650 | Dec. 6, 1650 | Flank (excentric) vent, regional fissure eruption, submarine eruption, new island formation, explosive eruption, lava flows, fatalities, damage, tsunami. |
| May 23, 1707 | Sep. 14, 1711 | Central vent eruption, regional fissure eruption, submarine eruption, new island formation, explosive eruption, lava flows, lava dome extrusion, damage. |
| Jan. 26, 1866 | Oct. 15, 1870 | Central vent eruption, regional fissure eruption, submarine eruption, new island formation, explosive eruption, lava flows, lava dome extrusion, fatalities, damage, evacuation. |
| Aug. 11, 1925 | Mar. 17, 1928 | Central vent eruption, regional fissure eruption, explosive eruption, phreatic explosions, lava flows, lava dome extrusion. |
| Aug. 20, 1939 | Jul. 2, 1941 ± 1 day | Central vent eruption, regional fissure eruption, submarine eruption, explosive eruption, phreatic explosions, lava flows, lava dome extrusion, damage. |
| Jan. 10, 1950 | Feb. 2, 1950 | Central vent eruption, regional fissure eruption, submarine eruption, explosive eruption, phreatic explosions, lava flows, lava dome extrusion. |
References
- ^ a b "Introduction – Santorini Volcano". Retrieved 2011-04-19.
- ^ "Tectonic setting of Santorini". Retrieved 2011-04-20.
- ^ "Geology of Santorini – The prevolcanic basement". Retrieved 2011-04-20.
- ^ J. Preine, J. Karstens, C. Hübscher, P. Nomikou, F. Schmid, G.J. Crutchley, T.H. Druitt and D. Papanikolaou "Spatio-temporal evolution of the Christiana-Santorini-Kolumbo volcanic field, Aegean Sea", doi=https://doi.org/10.1130/G49167.1
- ^ a b "Santorini". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-29.
- ^ "Santorini Volcanic Caldera, Greece". Retrieved 2011-04-19.
- ^ NBC News "Volcano on scenic Greek island getting a little restless 3 March 2012
- ^ Sparks, R. S. J. (2000). "Friedrich, W. L. 2000. Fire in the Sea. The Santorini Volcano: Natural History and the Legend of Atlantis". Geological Magazine. 137 (5). Cambridge University Press: 593. doi:10.1017/s0016756800224618. S2CID 128708746.
- ^ "Large Volcano Explocivity Index". Countries of the World. Archived from the original on 2020-09-30. Retrieved 2021-04-17.
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