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Kostakan

Kerucut piroklastik · Russia · 1150 m

A N-S-trending chain of scoria cones lies in the Kostakan valley south of Bakening volcano. The 600-year-old Glavny scoria cone (left center) is surrounded by its lava flow, which dammed a small river to form beautiful Kostakan lake. Two small vegetated early Holocene cones lie along the opposite side of the lake.
A N-S-trending chain of scoria cones lies in the Kostakan valley south of Bakening volcano. The 600-year-old Glavny scoria cone (left center) is surrounded by its lava flow, which dammed a small river to form beautiful Kostakan lake. Two small vegetated early Holocene cones lie along the opposite side of the lake. · Foto: Copyrighted photo by Sergei Konyaev (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
Tipe
Kerucut piroklastik
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Ketinggian
1150 m
Koordinat
53.833, 158.052
Letusan terakhir
1350
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Minor (Basaltic)
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

A group of basaltic cinder cones lies south of Bakening volcano, west of the Srednaya Avacha (Middle Avacha) river valley. They are part of a broad zone of regional late Pleistocene to Holocene basaltic volcanism west of the Eastern volcanic zone of Kamchatka that extends from the Kostakan Lake area to the south. Several of the cinder cones are breached by lava flows, some of which extend into the Srednaya Avacha valley. The highest-elevation vent, Zmeya crater, was constructed within a landslide scarp. An unnamed maar is located about 2 km S of Kostakan Lake. Eruptions have occurred during two time periods, between about 11,000 to 7,000 years ago and between about 1,200 and 600 years ago.

Ringkasan Wikipedia

Ringkasan Inggris

Kostakan is a north-south trending chain of cinder cones located in the southern part of the Kamchatka Peninsula, Russia.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
8050 BCE~7737 BCE · 1 letusan · VEI maks. 36797 BCE~6483 BCE · 1 letusan · VEI maks. 3723~1037 · 2 letusan · VEI maks. 31037~1350 · 2 letusan · VEI maks. 28050 BCE5857 BCE3350 BCE1157 BCE1037

Garis waktu rinci

  1. 1350VEI 1Perkiraan geologi
    1350 – Berlangsung
    Glavny
  2. 1200 (±50 tahun)VEI 2Perkiraan geologi
    1200 – Berlangsung
    Glavny
  3. 1000 (±50 tahun)VEI 3Perkiraan geologi
    1000 – Berlangsung
    Serpovidny
  4. 800 (±50 tahun)VEI 3Perkiraan geologi
    800 – Berlangsung
    Maar S of Lake Kostakan, Krasny cone
  5. 6550 SM (±500 tahun)VEI 3Perkiraan geologi
    BCE 6550 – Berlangsung
    Ochkovy
  6. 8050 SM (±1000 tahun)VEI 3Perkiraan geologi
    BCE 8050 – Berlangsung
    Domashnii

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.