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Shikotsu

Photo of this volcano
  • Country
  • Volcanic Region
  • Landform | Volc Type
  • Last Known Eruption
  • 42.688°N
  • 141.38°E

  • 1,320 m
    4,331 ft

  • 285040
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

Photo Gallery

Tarumai volcano, seen here from the SW contains a flat-topped lava dome that formed during an eruption in 1909. The dome was emplaced within a small caldera at the summit that formed during major explosive eruptions in 1667 and 1739 CE.

Photo by Tom Simkin, 1981 (Smithsonian Institution).
The flat-topped lava dome at the summit of Tarumai volcano was formed during an eruption in 1909. Frequent explosive eruptions took place from January 11 until April. On April 19 the new lava dome appeared. The dome grew to a height of 130 m and a width of 450 m. This 1981 photo views the dome from the NE.

Copyrighted photo by Katia and Maurice Krafft, 1981.
A 130-m-high lava dome was emplaced at the summit of Tarumai volcano on Hokkaido in 1909. The dome grew rapidly near the end of an explosive eruption that began on January 1. An eruption in 1917 produced the fissure that cuts diagonally across the dome. Subsequent eruptions have occurred along this fissure and at other locations on the summit and flanks of the dome.

Copyrighted photo by Katia and Maurice Krafft, 1981.
This face-like feature is formed by fissures cutting across a lava dome at the summit of Tarumai volcano on the northern Japanese island of Hokkaido. Two sets of fissures transect the dome, the one trending N30W (lower right) forming the "nose," and the other trending N60E. The lava dome dates to an eruption in 1909. The N60E fissure was formed during an eruption in 1917; later localized eruptions formed the "eyes."

Copyrighted photo by Katia and Maurice Krafft, 1981.
Tarumai volcano was constructed on the SE rim of the 13 x 15 km Shikotsu caldera. The summit has a small 1.5-km-wide caldera that formed during eruptions in 1667 and 1739 CE. It contains a flat-topped summit lava dome that was extruded in 1909. Two other Holocene post-caldera volcanoes occur at Shikotsu, Fuppushi (adjacent to Tarumai) and Eniwa, on the opposite side of the caldera.

Photo by Ichio Moriya (Kanazawa University).
Shikotsu caldera, seen from the SE with Yoteizan volcano on the horizon, is a 13 x 15 km caldera filled by Lake Shikotsu. Following formation of the caldera more than 30,000 years ago, three small cones were constructed along a NW-trend across the caldera. Snow-capped Tarumai (left center) formed near the SE rim of the caldera, along with Fuppushi to its right. A third volcano, Eniwa, was constructed on the NW caldera rim at the far side of the lake.

Photo by Ichio Moriya (Kanazawa University).
These thick pyroclastic flow deposits were produced during the major eruption that formed the 13 x 15 km Shikotsu caldera. The eruption produced 125 km3 of rhyolite tephra and pyroclastic flows. Pyroclastic flows traveled as far as 40 km, reaching the Pacific coast over a broad area. This outcrop is located 15 km ENE of the caldera.

Photo by Ryuta Furukawa, 1993 (Hokkaido University).
The 14 x 12 km Shikotsu caldera is shown in this September 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 28 km across). Tarumae is the cone on the SE rim of the caldera with a roughly 1.5-km-wide crater containing a lava dome. Between Tarumae and the caldera lake is the eroded Fuppushi cone. On the opposite (NW) side of the caldera is the Eniwa cone.

Satellite image courtesy of Planet Labs Inc., 2019 (https://www.planet.com/).