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Gunung Kizimen

Kizimen

Stratovolkan · Russia · 2334 m

Kizimen is seen here from the NW. The Holocene edifice is composed of closely spaced lava domes, lava flows, and pyroclastic-flow deposits. A faint plume from fumaroles are seen on the northern slope near the summit.
Kizimen is seen here from the NW. The Holocene edifice is composed of closely spaced lava domes, lava flows, and pyroclastic-flow deposits. A faint plume from fumaroles are seen on the northern slope near the summit. · Foto: Copyrighted photo by Vikto Dvigalo (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm). · Wikimedia Commons
Tipe
Stratovolkan
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Ketinggian
2334 m
Koordinat
55.131, 160.320
Letusan terakhir
2013
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

Kizimen is an isolated, conical stratovolcano that is morphologically similar to St. Helens prior to its 1980 eruption. The summit consists of overlapping lava domes, and blocky lava flows descend the flanks of the volcano, which is the westernmost of a volcanic chain north of Kronotsky volcano. The 2334-m-high edifice was formed during four eruptive cycles beginning about 12,000 years ago and lasting 2000-3500 years. The largest eruptions took place about 10,000 and 8300-8400 years ago, and three periods of long-term lava dome growth have occurred. The latest eruptive cycle began about 3000 years ago with a large explosion and was followed by intermittent lava dome growth lasting about 1000 years. An explosive eruption about 1100 years ago produced a lateral blast and created a 1.0 x 0.7 km wide crater breached to the NE, inside which a small lava dome (the fourth at Kizimen) has grown. Prior to 2010, only a single explosive eruption, during 1927-28, had been recorded in historical time.

Ringkasan Wikipedia

Gunung Kizimen adalah sebuah gunung berapi kerucut aktif di bagian selatan Semenanjung Kamchatka, Rusia.

Wikipedia · CC BY-SA · Baca artikel lengkap

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
8050 BCE~7715 BCE · 1 letusan · VEI maks. 56709 BCE~6373 BCE · 1 letusan · VEI maks. 56038 BCE~5703 BCE · 1 letusan · VEI maks. ?4697 BCE~4361 BCE · 1 letusan · VEI maks. 44361 BCE~4026 BCE · 1 letusan · VEI maks. 21343 BCE~1008 BCE · 1 letusan · VEI maks. ?333~669 · 1 letusan · VEI maks. ?669~1004 · 2 letusan · VEI maks. 31675~2010 · 2 letusan · VEI maks. 38050 BCE5703 BCE3020 BCE673 BCE1675

Garis waktu rinci

  1. 2010VEI 3Teramati
    2010-11-11 – 2013-09-13
    SE flank fissure
  2. 1927VEI 2Teramati
    1927-12 – 1928-01
  3. 850VEI 3Perkiraan geologi
    850 – Berlangsung
  4. 700 (±50 tahun)VEI ?Perkiraan geologi
    700 – Berlangsung
  5. 350 (±75 tahun)VEI ?Perkiraan geologi
    350 – Berlangsung
  6. 1010 SMVEI ?Perkiraan geologi
    BCE 1010 – Berlangsung
  7. 4050 SMVEI 2Perkiraan geologi
    BCE 4050 – Berlangsung
  8. 4450 SMVEI 4Perkiraan geologi
    BCE 4450 – Berlangsung
  9. 5800 SM (±50 tahun)VEI ?Perkiraan geologi
    BCE 5800 – Berlangsung
  10. 6400 SM (±50 tahun)VEI 5Perkiraan geologi
    BCE 6400 – Berlangsung
  11. 8050 SMVEI 5Perkiraan geologi
    BCE 8050 – Berlangsung

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.