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Selandia Baru · Stratovolkan

Rumble V Seamount

Rumble V

Tipe
Stratovolkan
Ketinggian
400 m (bawah laut)
Letusan terakhir
Tidak diketahui
A bathymetric map view shows Rumble V submarine volcano at the southern end of the South Kermadec volcano group. A large plume of gas bubbles was acoustically detected rising from the summit in 1992. Rumble V, the southernmost of a group of seamounts on the southern Kermadec Ridge known as the Rumbles, rises more than 2,000 m to about 400 m below the sea surface.
A bathymetric map view shows Rumble V submarine volcano at the southern end of the South Kermadec volcano group. A large plume of gas bubbles was acoustically detected rising from the summit in 1992. Rumble V, the southernmost of a group of seamounts on the southern Kermadec Ridge known as the Rumbles, rises more than 2,000 m to about 400 m below the sea surface. · Foto: Courtesy of Ian Wright (National Institute of Water and Atmospheric Research (NIWA), Wellington, New Zealand).
Tipe
Stratovolkan
Negara
Selandia Baru
Wilayah
Tonga & Kermadec / Southern Kermadec Volcanic Arc
Ketinggian
400 m (bawah laut)
Koordinat
-36.142, 178.196
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona subduksi / Kerak samudra (< 15 km)
Bentuk lahan
Komposit
Batuan utama
Andesit / Andesit basaltik
Ringkasan geologi

Rumble V was discovered in 1992 at the southernmost end of the Rumble seamounts on the southern Kermadec Ridge, 17 km ESE of Rumble IV. Andesitic and basaltic andesite rocks have been dredged from this volcano, which rises more than 2,000 m to nearly 400 m below the ocean surface and shows a pristine morphology. A large plume of gas bubbles was acoustically detected rising from the summit in 1992, and subsequent expeditions detected evidence of vigorous hydrothermal activity.

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