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Mount Haku

Hakusan

Stratovolcano · Japan · 2702m

Hakusan, seen here from the WNW, contains multiple vents along a roughly N-S line. Holocene eruptions have consisted of phreatic or phreatomagmatic explosions from several summit craters. Partial collapse of the summit produced a debris avalanche down the E flank. Eruptions were recorded over almost a thousand-year period until the 17th century.
Hakusan, seen here from the WNW, contains multiple vents along a roughly N-S line. Holocene eruptions have consisted of phreatic or phreatomagmatic explosions from several summit craters. Partial collapse of the summit produced a debris avalanche down the E flank. Eruptions were recorded over almost a thousand-year period until the 17th century. · Photo: Photo by Ishikawa Prefecture, 1994 (courtesy Toshio Higashino, Haku-san Nature Conservation Center). · Wikimedia Commons
Type
Stratovolcano
Country
Japan
Region
Western Pacific Volcanic Regions / Nankai Volcanic Arc
Elevation
2702m
Coordinates
36.155, 136.771
Last eruption
1659
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Andesite / Basaltic Andesite
Geological summary

Hakusan is a complex andesitic-dacitic stratovolcano near the western coast of central Honshu. It was constructed over a high basement of sedimentary rocks in a region of very heavy snowfall that has contributed to erosional dissection. Holocene eruptions have consisted of phreatic or phreatomagmatic explosions from several summit craters. Partial collapse of the summit produced a debris avalanche down the E flank during the mid-Holocene. Eruptions were recorded over almost a thousand-year period until the 17th century.

From Wikipedia

Mount Haku , or Mount Hakusan, is a dormant stratovolcano in Japan. It is located on the borders of Gifu and Ishikawa, on the island of Honshu. Mount Haku is thought to have first been active 300,000 to 400,000 years ago, with the most recent eruption occurring in 1659. Along with Mount Tate and Mount Fuji, it is one of Japan's "Three Holy Mountains" .

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Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
7550 BCE~7243 BCE · 1 eruptions · max VEI ?7243 BCE~6936 BCE · 1 eruptions · max VEI ?6629 BCE~6322 BCE · 1 eruptions · max VEI ?5094 BCE~4787 BCE · 1 eruptions · max VEI ?4173 BCE~3866 BCE · 1 eruptions · max VEI ?3559 BCE~3252 BCE · 1 eruptions · max VEI ?2639 BCE~2332 BCE · 1 eruptions · max VEI ?490 BCE~183 BCE · 1 eruptions · max VEI 4124~431 · 1 eruptions · max VEI ?431~738 · 2 eruptions · max VEI ?738~1045 · 5 eruptions · max VEI 31045~1352 · 2 eruptions · max VEI 31352~1659 · 7 eruptions · max VEI 37550 BCE5401 BCE2945 BCE797 BCE1352

Detailed timeline

  1. 1659VEI 2Observed
    1659-04-21 – 1659-08-08
    Midoriga-ike
  2. 1658VEI 2Observed
    1658-10 – Ongoing
  3. 1582VEI 2Observed
    1582 – Ongoing
  4. 1579VEI 3Observed
    1579-09-27 – Ongoing
    Jigoku-no-oana
  5. 1554VEI 3Observed
    1554-05 – 1556
    SW of Midoriga-ike
  6. 1548VEI 3Observed
    1548 – Ongoing
  7. 1547VEI 3Observed
    1547-03-04 – 1547-10
  8. 1239VEI 3Observed
    1239 – Ongoing
  9. 1177VEI 3Geological estimate
    1177-05-18 – Ongoing
  10. 1042VEI 3Observed
    1042 – Ongoing
    Midoriga-ike
  11. 900VEI ?Geological estimate
    900 – Ongoing
  12. 884VEI ?Geological estimate
    884 – Ongoing
  13. 859VEI ?Geological estimate
    859 – Ongoing
  14. 853VEI ?Geological estimate
    853 – Ongoing
  15. 706VEI ?Observed
    706-09 – Ongoing
  16. 500 (±100 yrs)VEI ?Geological estimate
    500 – Ongoing
  17. 200VEI ?Geological estimate
    200 – Ongoing
  18. 200 BCEVEI 4Geological estimate
    BCE 200 – Ongoing
    Kengamine
  19. 2550 BCE (±150 yrs)VEI ?Geological estimate
    BCE 2550 – Ongoing
  20. 3550 BCE (±500 yrs)VEI ?Geological estimate
    BCE 3550 – Ongoing
  21. 3900 BCE (±200 yrs)VEI ?Geological estimate
    BCE 3900 – Ongoing
  22. 5000 BCEVEI ?Geological estimate
    BCE 5000 – Ongoing
  23. 6550 BCE (±50 yrs)VEI ?Geological estimate
    BCE 6550 – Ongoing
  24. 7050 BCE (±500 yrs)VEI ?Geological estimate
    BCE 7050 – Ongoing
  25. 7550 BCE (±50 yrs)VEI ?Geological estimate
    BCE 7550 – Ongoing

External links

⚠ For reference only. Not for emergency response.