Isole Matthew e Hunter
Matthew Island
Stratovulcano · France - claimed by Vanuatu · 177 m
- Tipo
- Stratovulcano
- Paese
- France - claimed by Vanuatu
- Regione
- Pacifico sud-occidentale / Vanuatu Volcanic Arc
- Altitudine
- 177 m
- Coordinate
- -22.330, 171.320
- Ultima eruzione
- 1956
- Contesto tettonico
- Subduction zone / Crustal thickness unknown
- Forma vulcanica
- Composite
- Roccia principale
- Andesite / Basaltic Andesite
Sintesi geologica
Matthew Island is composed of two low andesitic-to-dacitic cones separated by a narrow isthmus. The Matthew name originates from an English mariner who sighted the island in 1788. Only the triangular eastern portion of the 0.6 x 1.2 km island was present prior to the 1940s, when construction of the larger western segment began; it consists primarily of lava flows. The western cone contains a crater that is breached to the NW and is filled by a lava flow whose terminus forms the NW coast.
Sintesi da Wikipedia
Riassunto in ingleseMatthew Island and Hunter Island are two uninhabited volcanic islands in the South Pacific, 300 kilometres (190 mi) east of New Caledonia and south-east of Vanuatu. The pair, which lie 70 km (43 mi) apart, are claimed by Vanuatu as part of Tafea Province, and considered by the people of Aneityum part of their custom ownership, but also claimed by France as part of New Caledonia.
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Storia delle eruzioni
Cronologia dettagliata
- 1976VEI 1Stima geologica1976-11-27 – In corso
- 1966VEI ?Stima geologica1966-08-16 – In corso
- 1963VEI 0Osservata1963-09-11 – 1964-07-02Norfolk Island Ridge
- 1956 (±2 anni)VEI 0Osservata1956-07-02 – In corsoWest-Matthew
- 1954VEI 2Osservata1954-10-16 – In corsoWest-Matthew (October 1954, not 1953)
- 1949VEI 2Osservata1949-07-02 – In corsoWest-Matthew
- 1828VEI ?Stima geologica1828-01-16 – In corso
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.