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Vanuatu · Stratovolkan

Eastern Gemini Seamount

Gemini-Oscostar

Tipe
Stratovolkan
Ketinggian
33 m (bawah laut)
Letusan terakhir
1996
Tipe
Stratovolkan
Negara
Vanuatu
Wilayah
Pasifik Barat Daya / Vanuatu Volcanic Arc
Ketinggian
33 m (bawah laut)
Koordinat
-20.957, 170.130
Letusan terakhir
1996
Kondisi tektonik
Zona rift / Kerak samudra (< 15 km)
Bentuk lahan
Gugusan gunung api
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

The submarine Gemini-Oscostar volcanic field lies near the southern end of the Vanuatu (or New Hebrides) Volcanic Arc, ~100 km S of Aneityum Island. Water discoloration and bursts of very dark water were observed from Oscostar seamount (also known as Eastern Gemini) from a passing ship on 18 February 1996. Overflights as late as 22 February noted periodic explosions that ejected black material to about 20 m above sea level. It consists of an elongated NNE-SSW-trending ridge of submarine volcanoes with satellitic cones. Several basaltic samples and one andesitic rock dredged in 1989 were described as glassy, vesicular, and extremely fresh.

Ringkasan Wikipedia

Ringkasan Inggris

The Eastern Gemini Seamount, also known as Oscostar, is a seamount in the southwestern Pacific Ocean, about halfway between Vanuatu's Tanna and Matthew Islands. The only recorded eruption from Eastern Gemini was observed by a passing ship on February 18, 1996 when bursts of very dark water were observed.

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1996~1996 · 1 letusan · VEI maks. 119961996199719971997

Garis waktu rinci

  1. 1996VEI 1Teramati
    1996-02-18 – 1996-02-22

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