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Mount Taishaku

Omanago Group

Lava dome · Japan · 2341m

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. · Photo: Photo by Lee Siebert, 1964 (Smithsonian Institution). · Wikimedia Commons
Type
Lava dome
Country
Japan
Region
Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
Elevation
2341m
Coordinates
36.807, 139.476
Last eruption
-3050
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Cluster
Major rock type
Dacite
Geological summary

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.

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
3050 BCE~3050 BCE · 1 eruptions · max VEI ?3050 BCE3050 BCE3049 BCE3049 BCE3049 BCE

Detailed timeline

  1. 3050 BCEVEI ?Geological estimate
    BCE 3050 – Ongoing
    Mitsu-dake

External links

⚠ For reference only. Not for emergency response.