Mount Kusatsu-Shirane
Kusatsu-Shiranesan
Stratovolcano · Japan · 2165m

- Type
- Stratovolcano
- Country
- Japan
- Region
- Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
- Elevation
- 2165m
- Coordinates
- 36.618, 138.528
- Last eruption
- 2018
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
The Kusatsu-Shiranesan complex, located immediately north of Asama volcano, consists of a series of overlapping pyroclastic cones and three crater lakes. The andesitic-to-dacitic volcano was formed in three eruptive stages beginning in the early to mid-Pleistocene. The Pleistocene Oshi pyroclastic flow produced extensive welded tuffs and non-welded pumice that covers much of the E, S, and SW flanks. The latest eruptive stage began about 14,000 years ago. Historical eruptions have consisted of phreatic explosions from the acidic crater lakes or their margins. Fumaroles and hot springs that dot the flanks have strongly acidified many rivers draining from the volcano. The crater was the site of active sulfur mining for many years during the 19th and 20th centuries.
From Wikipedia
Mount Kusatsu-Shirane is a 2,165 m (7,103 ft) active stratovolcano in Kusatsu, Gunma, Japan. It is called Kusatsu Shirane to differentiate it from the Mount Nikkō-Shirane on the other side of Gunma Prefecture. The summit of Kusatsu-Shirane volcano, located immediately north of Asama volcano, consists of a series of overlapping pyroclastic cones and three crater lakes. The largest of these is Yu-gama, an acidic emerald green lake with rafts of yellow sulfur sometimes seen floating on its surface.
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Eruption history
Detailed timeline
- 2018VEI 1Observed2018-01-23 – 2018-01-23Motoshiranesan
- 1989VEI 1Geological estimate1989-01-06 – 1989-01-06NW part of Yu-gama
- 1983VEI 1Observed1983-07-26 – 1983-12-21Yu-gama, Kara-gama
- 1982VEI 1Observed1982-10-26 – 1982-12-29Kara-gama, Yu-gama
- 1976VEI 1Observed1976-03-02 – 1976-03-02NE corner of Mizu-gama Crater
- 1958VEI 1Observed1958-12-31 – OngoingYu-gama
- 1942VEI 1Observed1942-02-02 – OngoingFissure east and south of Yu-gama
- 1941VEI 1Observed1941-01-19 – 1941-01-19
- 1940VEI 1Observed1940-04-07 – 1940-09-13
- 1939VEI 1Observed1939-02 – 1939-08-28Yu-gama
- 1938VEI 1Observed1938-07-17 – 1938-10-05Yu-gama
- 1937VEI 1Observed1937-11-27 – 1938-02-16Yu-gama
- 1934VEI 2Observed1934 – Ongoing
- 1933VEI ?Geological estimate1933 – Ongoing
- 1932VEI 3Observed1932-10-01 – 1932-11NE part of Yu-gama, SE outer rim
- 1927VEI 2Observed1927-12-29 – 1927-12-31N Yu-gama & S outer rim (in 1927, not 1928)
- 1925VEI 2Observed1925-01-22 – 1925-01-30Northern part of Yu-gama
- 1905VEI 2Observed1905-10 – 1905-10Yu-gama
- 1903VEI ?Geological estimate1903 – Ongoing
- 1902VEI 1Observed1902-07-15 – 1902-09-24North side of Yumi-ike
- 1900VEI 1Observed1900-10-01 – 1900-10-01NE part of Yu-gama
- 1897VEI 2Observed1897-07-08 – 1897-08-16NE part of Yu-gama
- 1882VEI 2Observed1882-08-06 – 1882-08-16Yu-gama, NE end of Kara-gama
- 1805VEI 2Observed1805 – OngoingYu-gama
- 1470 (±150 yrs)VEI ?Geological estimate1470 – Ongoing
- 50VEI 2Geological estimate50 – OngoingYu-gama
- 550 BCEVEI 3Geological estimateBCE 550 – OngoingYu-gama
- 1120 BCE (±150 yrs)VEI 4Geological estimateBCE 1120 – OngoingMoto-Shirane
- 3750 BCEVEI 2Geological estimateBCE 3750 – OngoingShirane
- 6270 BCE (±200 yrs)VEI ?Geological estimateBCE 6270 – Ongoing
- 6550 BCEVEI 3Geological estimateBCE 6550 – OngoingShirane
External links
⚠ For reference only. Not for emergency response.