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Unnamed volcano

Titan Ridge

Rekahan erupsi · Papua New Guinea · 1300 m (bawah laut)

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Tipe
Rekahan erupsi
Negara
Papua New Guinea
Wilayah
Pasifik Barat Daya / Bismarck Sea Volcanic Province
Ketinggian
1300 m (bawah laut)
Koordinat
-3.030, 147.780
Letusan terakhir
1972
Kondisi tektonik
Rift zone / Continental crust (> 25 km)
Bentuk lahan
Cluster
Batuan utama
No Data (checked)
Ringkasan geologi

SOFAR signals resembling those produced at known submarine eruptions were recorded in January 1972 in the central Bismarck Sea (Johnson et al., 1981). The source of the signals was at the junction of two segments of the N margin of the South Bismarck plate. The more easterly of these segments is a transform fault, whereas the more westerly is an area of oblique active seafloor spreading. The signals were detected by a seismic station on nearby Manus Island, as well as at hydrophone stations on Wake and Midway Islands in the central Pacific. During the eruption in 2026 the "Titan Ridge" name was proposed by local residents. The general story of the Titan (pronounced Tee-Tahn) people is that their island home got devastated and reduced to the Circular Reef (~40 km SSW) due to an uncertain natural phenomenon; they drifted for awhile before they settled, and most of the Titan villages are now mainly along the south coast of Manus Island.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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1972~1972 · 1 letusan · VEI maks. 019721972197319731973

Garis waktu rinci

  1. 1972VEI 0Teramati
    1972-01-08 – 1972-01-12

Tautan eksternal

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