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Inggris Raya · Stratovolkan

Nightingale Island

Tipe
Stratovolkan
Ketinggian
365 m
Letusan terakhir
2004
Nightingale Island
Foto: Brian Gratwicke from DC, USA · CC BY 2.0 · Wikimedia Commons
Tipe
Stratovolkan
Negara
Inggris Raya
Wilayah
Samudra Atlantik / Southern Atlantic Volcano Group
Ketinggian
365 m
Koordinat
-37.420, -12.480
Letusan terakhir
2004
Kondisi tektonik
Zona rift / Kerak samudra (< 15 km)
Bentuk lahan
Komposit
Batuan utama
Trakit / Trakidasit
Ringkasan geologi

Nightingale Island, along with the adjacent smaller Middle (or Alex) and Stoltenhoff Islands and associated small islets, are the southernmost of the Tristan da Cunha island group. The heavily eroded island consists of ash and agglomerate units with intervening massive trachytic intrusions and lava flows. Volcanic rocks were K-Ar dated at between 400,000 and 150,000 years, and a radiocarbon date of about 39,000 years BP was obtained from an ash layer overlain by a lava flow. An earthquake swarm lasting 6 hours beginning on 29 July 2004 was followed by observation of large blocks of floating phonolitic pumice that washed up on Tristan da Cunha. The pumice was considered to be from an eruption associated with an earthquake swarm 37-53 km SSE of Tristan da Cunha on the submarine SE flank of Nightingale Island.

Ringkasan Wikipedia

Ringkasan Inggris

Nightingale Island is an active volcanic island in the South Atlantic Ocean, 3 square kilometres (1.2 sq mi) in area, part of the Tristan da Cunha group of islands. They are administered by the United Kingdom as part of the overseas territory of Saint Helena, Ascension and Tristan da Cunha.

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2004~2004 · 1 letusan · VEI maks. 020042004200520052005

Garis waktu rinci

  1. 2004VEI 0Teramati
    2004-07-29 – 2004-07-30
    Submarine SE flank

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