East Epi (volcano): Difference between revisions
←Created page with '{{Short description|submarine volcano in Vanuatu}} {{Infobox seamount | name = East Epi | photo = ShadedmapEpi.jpg | photo_caption = Shaded relief map of the Epi caldera; Epi-A, Epi-B and Epi-C are marked. | depth = {{cvt|34|m|ft|0}} | prominence = | location = Vanuatu | range = | coordinates = {{Coord|16|40|48|S|168|22|12|E|display=inline,title}} | topo = | type = Caldera, cinder cones | age = | last_eruption = 2004 }} East of the Vanuatu i...' Tag: Disambiguation links added |
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Revision as of 23:19, 31 December 2022
| East Epi | |
|---|---|
 Shaded relief map of the Epi caldera; Epi-A, Epi-B and Epi-C are marked. | |
 | |
| Summit depth | 34 m (112 ft) |
| Location | |
| Location | Vanuatu |
| Coordinates | 16°40′48″S 168°22′12″E / 16.68000°S 168.37000°E |
| Geology | |
| Type | Caldera, cinder cones |
| Last eruption | 2004 |
East of the Vanuatu island of Epi can be found a series of active underwater volcanic cones and a caldera which last erupted in 2004. These series of submarine volcanoes are generally referred as East Epi, and the 3 bigger cones have specific names, from west to east, Epi-A, Epi-B and Epi-C. All of these cones have had intermittent activity in this and the last century.
Geography
These submarine volcanoes are located approximately 6 km east of Epi Island, 15 km south of Lopevi, an active volcano and 25 km north-northwest of Kuwae, another submarine volcano (caldera) between the islands of Epi and Tongoa.
Bathymetry
The Epi underwater seamount complex is made up of a possible submarine caldera with 3 bigger cones aligned on the northern rim of the caldera.[1] The Epi-A cone consists of a wide crater at the summit, with the highest point located 124 meter below sea level. Meanwhile, Epi-B has a summit of 34 meters and Epi-C has a highest point of 169 meters below sea level.[2]
Rock types
In a research done in 1988, basaltic and dacitic products were found emitted from the Epi-A and Epi-B cones.[1]
Geologic setting
The volcanoes are located in New Hebrides Island Arc which includes the Vanuatu Islands, which lie on the convergent plate boundary where the Australian Plate subducts (sinks) beneath the New Hebrides Plate. The subducting crust melts under the high pressure and temperatures which causes the formation of magma underground. The magma rises up onto the surface, which then forms a chain of volcanoes. These volcanoes allow the magma to be released into the air with several types of volcanic products.[3]
Eruptive history
The Epi caldera has 8 recorded eruptions over the Holocene period; in order, the volcano erupted in 1920, 1953, 1958, 1960, 1979, 1999, 2002 and 2004. There were unconfirmed eruptions with questionable certainty in November of 1953, 1971, 1972, 1973, 1974 and 1988. The biggest eruption out of all of these was in 1953, when the volcano had an eruption equivalent to 3 in the VEI scale.[4]
1953 eruption
One of the cones appeared over the sea level for a short time while big amounts of pumice were erupting from it.[1] Volcanic material was ejected into the air as high as 100 meters above the sea level and rafts of pumice covered an area of around 1,000 km².[4]
1958 eruption
It was the second largest ever recorded in the Epi Caldera with a VEI of 2. This eruption was sourced from the Epi-B cone and the eruption of the pumice causing discolored water was observed from an aircraft.[4]
2004 eruption
In early 2004, in the 16th of February, loud explosion noises were heard from Epi Island residents. Shortly after, a fishing vessel called Azur witnessed and recorded an explosion that breached the surface of the sea. Shortly after, officials were informed about the eruption which prompted them to gather witnesses for the eruption.[4]
The eruption lasted 6 days, and was later revealed that the eruption was caused by the Epi-B cone, similar to most recorded eruptions including 1958. A few months later, this prompted research to be done about the volcano and it's characteristics.[4]
See also
References
- ^ a b c Greene, H. G.; Exon, N. F. (1988). "Acoustic stratigraphy and hydrothermal activity within Epi Submarine Caldera, Vanuatu, New Hebrides Arc". Geo-Marine Letters. 8 (3): 121–129. doi:10.1007/BF02326088. Retrieved 31 December 2022.
- ^ Exon, N. F.; Cronan, D. S. (1983). "Hydrothermal iron deposits and associated sediments from submarine volcanoes off Vanuatu, southwest Pacific". Marine Geology. 52 (3–4): 43–52. doi:10.1016/0025-3227(83)90052-X. Retrieved 31 December 2022.
- ^ "Volcano Info". Vanuatu Meteorology and Geo-hazards Department. Retrieved December 31, 2022.
- ^ a b c d e "Epi". Global Volcanism Program. Smithsonian Institution. Retrieved 2022-12-31.