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Bogdan Khmelnitsky

Chirippusan [Chirip]

Stratovolcano · Japan - administered by Russia · 1587m

The Chirippusan Peninsula protrudes NW into the Sea of Okhotsk from central Iturup Island and is composed of two Holocene cones. Minamichirippusan (center) lies at the southern end of the peninsula and Chirippusan (in the background to the left) forms the northern end. Lava flows from Minamichirippusan reach the coast on both the E and W sides of the peninsula.
The Chirippusan Peninsula protrudes NW into the Sea of Okhotsk from central Iturup Island and is composed of two Holocene cones. Minamichirippusan (center) lies at the southern end of the peninsula and Chirippusan (in the background to the left) forms the northern end. Lava flows from Minamichirippusan reach the coast on both the E and W sides of the peninsula. · Photo: Photo by Alexander Rybin, 2001 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin). · Wikimedia Commons
Type
Stratovolcano
Country
Japan - administered by Russia
Region
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Elevation
1587m
Coordinates
45.338, 147.920
Last eruption
1860
Tectonic setting
Subduction zone / Intermediate crust (15-25 km)
Landform
Composite
Major rock type
Basalt / Picro-Basalt
Geological summary

Chirippusan (also simply Chirip) volcano is on the Chirip Peninsula, which extends N into the Sea of Okhotsk from central Iturup Island. The summits of two overlapping stratovolcanoes are ~4.5 km apart along a volcanic ridge, with Kitachirippusan on the north and Minamichirippu (also called Bogdan Khmelnitskii) on the south. Lava flows from both edifices are truncated by a large 4-km-wide depression on the west side of the peninsula. Basaltic rocks dominate at both volcanoes over basaltic andesite and andesitic products. Kitachirippusan has a shallow summit crater, partially filled by a small lake, that has fed lava flows down all sides; satellitic cones are located on the northern flank. Lava flows from Minamichirippusan reach the coast on both the east and west. Only two eruptions are known, one in 1843 CE and another in 1860 CE from a vent SE of the Minamichirippusan summit.

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1843~1845 · 1 eruptions · max VEI 21858~1860 · 1 eruptions · max VEI 118431846185218551858

Detailed timeline

  1. 1860VEI 1Observed
    1860 – Ongoing
    SE of Bogdan Khmelinitskii summit
  2. 1843VEI 2Observed
    1843 – Ongoing

External links

⚠ For reference only. Not for emergency response.