Lewati ke konten utama

Rusia · Gunung api perisai

Severny

Tipe
Gunung api perisai
Ketinggian
1936 m
Letusan terakhir
-1550
The red Tobeltsen scoria cone, seen from the SE, lies on the lower WSW flank of Severny erupted about 3,500 years ago and was the source of lava flows that descend diagonally to the lower left. Severny is a late-Quaternary volcano located at the NW end of a major NE-trending graben along the crest of the northern Sredinny Range.
The red Tobeltsen scoria cone, seen from the SE, lies on the lower WSW flank of Severny erupted about 3,500 years ago and was the source of lava flows that descend diagonally to the lower left. Severny is a late-Quaternary volcano located at the NW end of a major NE-trending graben along the crest of the northern Sredinny Range. · Foto: Copyrighted photo by Maria Pevzner, 2005 (Russian Academy of Sciences, Moscow).
Tipe
Gunung api perisai
Negara
Rusia
Wilayah
Pasifik Barat Laut / Central Kamchatka Volcanic Arc
Ketinggian
1936 m
Koordinat
58.280, 160.870
Letusan terakhir
-1550
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Perisai
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

Severny is a late Quaternary shield volcano located at the NW end of a major NE-trending graben along the crest of the northern Sredinny Range. It is capped by a small stratovolcano, a small shield volcano was constructed on its SW flank, and an even smaller shield grew on the NE flank. The basaltic Tobeltsen cinder cone on the WSW flank and associated lava flows were erupted about 3,500 years ago.

Riwayat letusan

1 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu · Gunakan tombol panah untuk berpindah batang, Enter untuk membuka
1550 SM~1550 SM · 1 letusan · VEI maks. ?1550 SM1550 SM1549 SM1549 SM1549 SM

Garis waktu rinci

  1. 1550 SMVEI ?Perkiraan geologi
    1550 SM – akhir tidak diketahui
    WSW flank (Tobeltsen)

Gunung api terdekat

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.