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Rusia · Kerucut lava

Bliznetsy

Tipe
Kerucut lava
Ketinggian
265 m
Letusan terakhir
-1060
Two closely spaced vents visible near the center of this photo produced the Bliznetsy ("Twins") lava flows. Prominent compressional ridges are visible on the flows, which were dated at about 3,000 years ago. Emplacement of the lava field was preceded by weak phreatomagmatic eruptions.
Two closely spaced vents visible near the center of this photo produced the Bliznetsy ("Twins") lava flows. Prominent compressional ridges are visible on the flows, which were dated at about 3,000 years ago. Emplacement of the lava field was preceded by weak phreatomagmatic eruptions. · Foto: Photo courtesy of Maria Pevzner (Russian Academy of Sciences, Moscow).
Tipe
Kerucut lava
Negara
Rusia
Wilayah
Pasifik Barat Laut / Central Kamchatka Volcanic Arc
Ketinggian
265 m
Koordinat
57.350, 161.370
Letusan terakhir
-1060
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Kecil
Batuan utama
Andesit / Andesit basaltik
Ringkasan geologi

The Bliznetsy ("Twins") lava flows occupy a low-lying area east of the Sredinny Range and north of the Eastern Volcanic Zone volcanoes. The young flows lie south of the Ozernaya River about 80 km north of historically active Sheveluch volcano. Effusion of about 0.5 km3 of lava flows about 3000 years ago was preceded by weak phreatomagmatic eruptions.

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1060 SM~1060 SM · 1 letusan · VEI maks. 11060 SM1060 SM1059 SM1059 SM1059 SM

Garis waktu rinci

  1. 1060 SM (±40 tahun)VEI 1Perkiraan geologi
    1060 SM – akhir tidak diketahui

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