Kolumbo
| Kolumbo | |
|---|---|
 | |
| Summit depth | −10 m (−30 ft) |
| Height | 400 m (1,312 ft) |
| Location | |
| Location | Aegean Sea |
| Coordinates | 36°31′00″N 25°29′30″E / 36.51667°N 25.49167°E |
| Country | Greece |
| Geology | |
| Type | Submarine volcano |
| Volcanic arc/chain | South Aegean Volcanic Arc |
| Last eruption | 1650 |
| History | |
| Discovery date | 1649 |
Kolumbo is an active submarine volcano in the Aegean Sea in Greece, about 8 km northeast of Cape Kolumbo, Santorini island. The largest of a line of about twenty submarine volcanic cones extending to the northeast from Santorini,[1] it is about 3 km in diameter with a crater 1.5 km across.[2] It was first noticed by humans when it breached the sea surface in 1649-50. The Smithsonian Institution's Global Volcanism Program treats it as part of the Santorini volcano,[3] though at least one source maintains that it is a separate magmatic system.[4]
History
[edit]An eruption in 1650, which occurred when the accumulating cone reached the surface, sent pyroclastic flows across the sea surface to the shores and slopes of Santorini, where about seventy people and many animals died. A small ring of white pumice that formed was rapidly eroded away by wave action. The volcano collapsed into its caldera, triggering a tsunami that caused damage on nearby islands up to 150 km distant.[5] The highest parts of the crater rim are now about 10 m below sea level.
In 2006, sea floor pyroclastic deposits from the two Aegean explosions were explored, sampled and mapped by an expedition by NOAA Ocean Explorer, equipped with ROV robotics.
The crater floor, averaging about 505 m below the sea surface, is marked in its northeast area by a field of hydrothermal vents and covered by a thick bacterial community, the 2006 NOAA expedition discovered. Superheated (measured as hot as 224 °C) metal-enriched water issuing from the vents has built chimneys of polymetallic sulfide/sulfates to a maximum height of 4 m, apparently accumulated since the 1650 event.
The 2006 expedition initiated new seismic air-gun techniques in order to determine the volume and distribution of the submarine volcanic deposit of pumice and ash on the sea floor around Santorini, which has been studied extensively since 1975. Revised, more accurate estimates of the total dense rock equivalent volume of the Minoan event(s), consisting of pyroclastic sea floor deposits, distal ash fallout and ignimbrites on the island of Santorini, is likely about 60 km3, a greatly increased estimate,[6] comparable to the largest historic explosion, Mount Tambora 1815; the increased estimate affects the size of the ensuing tsunami as it has been widely modeled.
In October 2022 it was announced that a previously undetected magma chamber had been discovered approximately 2 to 4 km below sea level in the Kolumbo underwater volcano. Scientists had determined that it is gradually filling with melt. Although an eruption is not imminent, it does pose a threat which has prompted them to recommend real-time monitoring of the volcano.[7]
See also
[edit]Notes
[edit]- ^ Ref. University of Rhode Island: Kolumbo
- ^ Most of the information in this article is derived from the on-line reports of the NOAA Ocean Explorer, in References.
- ^ "Santorini". Global Volcanism Program. Smithsonian Institution. Retrieved 2017-07-12.
- ^ Klaver, Martijn; Carey, Steven; Nomikou, Paraskevi; Smet, Ingrid; Godelitsas, Athanasios; Vroon, Pieter (2016). "A distinct source and differentiation history for Kolumbo submarine volcano, Santorini volcanic field, Aegean arc". Geochemistry, Geophysics, Geosystems. 17 (8). American Geophysical Union: 3254–3273. Bibcode:2016GGG....17.3254K. doi:10.1002/2016GC006398. PMC 5114867. PMID 27917071.
- ^ Ref. University of Rhode Island: Kolumbo; Fouqué 1879
- ^ Compare Sigurdsson et al. 1990.
- ^ Chrapkiewicz, K.; Paulatto, M.; Heath, B. A.; Hooft, E. E. E.; Nomikou, P.; Papazachos, C. B.; Schmid, F.; Toomey, D. R.; Warner, M. R.; Morgan, J. V. (2022). "Magma Chamber Detected Beneath an Arc Volcano With Full-Waveform Inversion of Active-Source Seismic Data". Geochemistry, Geophysics, Geosystems. 23 (11). American Geophysical Union. Bibcode:2022GGG....2310475C. doi:10.1029/2022GC010475. S2CID 253104406.
References
[edit]- NOAA Ocean Explorer: Thera 2006 Expedition Summary
- NOAA Ocean Explorer: Thera 2006 Expedition detailed Log
- University of Rhode Island: Kolumbo Volcano
- Ferdinand André Fouqué, Santorin et ses éruptions (Paris: Masson) 1879.
- Haraldur Sigurdsson, S. Carey, C. Mandeville, 1990. "Assessment of mass, dynamics and environmental effects of the Minoan eruption of the Santorini volcano" in Thera and the Aegean World III: Proceedings of the Third Thera Conference, vol II, pp 100–12.
- Haraldur Sigurdsson and S. Carey "Marine investigations of Greece's Santorini volcanic field" (on-line text) Sigurdsson and Carey's revised estimate.
Further reading
[edit]- Kilias, S.P., Nomikou, P., Papanikolaou, D., Polymenakou, P.N., Godelitsas, A., Argyraki, A., Carey, S., Gamaletsos, P., Mertzimekis, T.J., Stathopoulou, E., Goettlicher, J., Steininger, R., Betzelou, K., Livanos, I., Christakis, Ch., Croff Bell, K., Scoullos, M. (2013). New insights into hydrothermal vent processes in the unique shallow-submarine arc-volcano, Kolumbo (Santorini), Greece. Scientific Reports 3. doi:10.1038/srep02421
- Preine, J.; Karstens, K.; Hübscher, C.; Nomikou, P.; Schmid, F.; Crutchley, G.J.; Druitt, T.H.; Papanikolaou, D. (2021). "Spatio-temporal evolution of the Christiana-Santorini-Kolumbo volcanic field, Aegean Sea". Geology. 50. Boulder, CO: Geological Society of America: 96–100. doi:10.1130/G49167.1. S2CID 241834116.
- Vougioukalakis, G., A. Sbrana and D. Mitropoulos, 1995. "The 1649-50 Kolumbo submarine volcano activity, Santorini, Greece," in F. Barberi, R. Casale, M. Fratta, (eds.) The European Laboratory Volcanoes: Workshop Proceeding (Luxembourg: EC European Science Commission) pp 189–92.
External links
[edit]
Media related to Kolumbo at Wikimedia Commons