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Bogdan Khmelnitsky

Chirippusan [Chirip]

Stratovolkan · Japan - administered by Russia · 1587 m

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. · Foto: Photo by Alexander Rybin, 2001 (Institute of Marine Geology and Geophysics, Yuzhno-Sakhalin). · Wikimedia Commons
Tipe
Stratovolkan
Negara
Japan - administered by Russia
Wilayah
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Ketinggian
1587 m
Koordinat
45.338, 147.920
Letusan terakhir
1860
Kondisi tektonik
Subduction zone / Intermediate crust (15-25 km)
Bentuk lahan
Composite
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

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.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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1843~1845 · 1 letusan · VEI maks. 21858~1860 · 1 letusan · VEI maks. 118431846185218551858

Garis waktu rinci

  1. 1860VEI 1Teramati
    1860 – Berlangsung
    SE of Bogdan Khmelinitskii summit
  2. 1843VEI 2Teramati
    1843 – Berlangsung

Tautan eksternal

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