Kostakan
Kerucut piroklastik · Russia · 1150 m

- 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 InggrisKostakan is a north-south trending chain of cinder cones located in the southern part of the Kamchatka Peninsula, Russia.
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
Garis waktu rinci
- 1350VEI 1Perkiraan geologi1350 – BerlangsungGlavny
- 1200 (±50 tahun)VEI 2Perkiraan geologi1200 – BerlangsungGlavny
- 1000 (±50 tahun)VEI 3Perkiraan geologi1000 – BerlangsungSerpovidny
- 800 (±50 tahun)VEI 3Perkiraan geologi800 – BerlangsungMaar S of Lake Kostakan, Krasny cone
- 6550 SM (±500 tahun)VEI 3Perkiraan geologiBCE 6550 – BerlangsungOchkovy
- 8050 SM (±1000 tahun)VEI 3Perkiraan geologiBCE 8050 – BerlangsungDomashnii
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.