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Tatun Volcano Group

Tatun Volcanic Group

Duomo di lava · Taiwan · 1120 m

The Tatun (Datun) volcano group contains around 20 lava domes and is seen here NE of Taipei, the capital city of Taiwan. The latest eruptions are late Pleistocene and mid-Holocene. Hot springs, fumaroles, and solfataras are found over wide areas.
The Tatun (Datun) volcano group contains around 20 lava domes and is seen here NE of Taipei, the capital city of Taiwan. The latest eruptions are late Pleistocene and mid-Holocene. Hot springs, fumaroles, and solfataras are found over wide areas. · Foto: Photo by Alexander Belousov, 2008 (Institute of Volcanology, Kamchatka, Russia). · Wikimedia Commons
Tipo
Duomo di lava
Paese
Taiwan
Regione
Western Pacific Volcanic Regions / Ryukyu Volcanic Arc
Altitudine
1120 m
Coordinate
25.178, 121.553
Ultima eruzione
648
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Cluster
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

The Tatun (Datun) group consists predominately of a series of andesitic lava domes in the northernmost part of Taiwan. About 20 volcanoes, the southernmost of which is only 15 km N of the capital city of Taipei, are included in the Tatun group, which was constructed along E-W and NE-SW trending ridges. The highest and youngest volcano is the Cising (Chisingshan) lava dome. Several magmatic eruptions took place in the group about 23,000 to 13,000 years ago, and a phreatic eruption associated with collapse of the lava dome, possibly closely following lava effusion, took place about 6,000 years ago. Hot springs, fumaroles, and solfataras are found over wide areas along a zone parallel to the SW-NE-trending Chinshan fault and extending to the NE coast of Taiwan, and extensive geothermal exploration has occurred at the Daiton geothermal area.

Sintesi da Wikipedia

Riassunto in inglese

The Tatun Volcanic Group or Tatun Volcano Group (TVG) constitutes a group of volcanoes located in northern Taiwan. It is located 15 km north of Taipei, and lies to the west of Keelung. It just adjoins the northern coast of the Taiwan island. The volcanic group was a result of episodic volcanism between 2.8 and 0.2 Ma. Research in the 2020s suggest that there were eruptions more recently than 0.2 Ma. The last eruption occurred in the year 648.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
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4095 BCE~3897 BCE · 1 eruzioni · VEI max. 1450~648 · 1 eruzioni · VEI max. 04095 BCE2909 BCE1723 BCE735 BCE450

Cronologia dettagliata

  1. 648 (±11 anni)VEI 0Stima geologica
    648 – In corso
    Shamao
  2. 4095 a.C. (±35 anni)VEI 1Stima geologica
    BCE 4095 – In corso
    Cisingshan

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.