Bogdan Khmelnitsky
Chirippusan [Chirip]
Stratovolkan · Japan - administered by Russia · 1587 m
- 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
Garis waktu rinci
- 1860VEI 1Teramati1860 – BerlangsungSE of Bogdan Khmelinitskii summit
- 1843VEI 2Teramati1843 – Berlangsung
Tautan eksternal
- Belum ada di Wikipedia (Bahasa Indonesia). Anda dapat berkontribusi di Wikidata.
- 🔗 Halaman asli Smithsonian GVP
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.