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Mount Taishaku

Omanago Group

Kubah lava · Japan · 2341 m

The Omanago volcano group (upper left) consists of a series of five lava domes in Nikko National Park. The highest dome is Omanago, located at the SE end of the complex. Mitsudake is the NW-most dome. The higher northern peak of the Mitsudake complex is out of view to the left, and the lower southern dome forms the low ridge behind the hot spring resort of Yunoko lake in the center of the photo. The peak on the right horizon is Nantaisan.
The Omanago volcano group (upper left) consists of a series of five lava domes in Nikko National Park. The highest dome is Omanago, located at the SE end of the complex. Mitsudake is the NW-most dome. The higher northern peak of the Mitsudake complex is out of view to the left, and the lower southern dome forms the low ridge behind the hot spring resort of Yunoko lake in the center of the photo. The peak on the right horizon is Nantaisan. · Foto: Photo by Lee Siebert, 1964 (Smithsonian Institution). · Wikimedia Commons
Tipe
Kubah lava
Negara
Japan
Wilayah
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
Ketinggian
2341 m
Koordinat
36.807, 139.476
Letusan terakhir
-3050
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Cluster
Batuan utama
Dacite
Ringkasan geologi

The Omanago volcano group consists of a series of five closely spaced lava domes that were constructed north and NW of Nantai volcano in Nikko National Park. The highest of the dacitic domes is Omanago, which later erupted andesitic lavas. The Mitsudake dome, which overlooks the hot spring resort of Lake Yunoko, was radiocarbon dated at about 5,000 years ago. Mitsudake was constructed on a southerly dipping slope, so that the southern of its two flat-topped domes is lower, and is overlapped by sediments of the Senjogahara plain.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
3050 BCE~3050 BCE · 1 letusan · VEI maks. ?3050 BCE3050 BCE3049 BCE3049 BCE3049 BCE

Garis waktu rinci

  1. 3050 SMVEI ?Perkiraan geologi
    BCE 3050 – Berlangsung
    Mitsu-dake

Tautan eksternal

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