Unnamed volcano
Titan Ridge
割れ目火口 · Papua New Guinea · 1300m (海底)
- タイプ
- 割れ目火口
- 国
- Papua New Guinea
- 地域
- 南西太平洋 / Bismarck Sea Volcanic Province
- 標高
- 1300m (海底)
- 座標
- -3.030, 147.780
- 最終噴火
- 1972年
- テクトニクス環境
- Rift zone / Continental crust (> 25 km)
- 火山地形
- Cluster
- 主要岩石
- No Data (checked)
地質学的概要
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.
噴火履歴
詳細タイムライン
- 1972年VEI 0観測記録1972-01-08 ~ 1972-01-12
外部リンク
- 日本語版Wikipediaには未登録です。Wikidataで作成できます。
- 🔗 Smithsonian GVP 原典ページ
⚠ 参考情報です。緊急対応には使用しないでください。