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Ostry

Stratovolkan · Russia · 2552 m

Snow-capped Ostry is seen here from the NW. On the right horizon is an unnamed cone on the SW flank of Ostry, which erupted about 4,000 years ago producing a basaltic lava flow.
Snow-capped Ostry is seen here from the NW. On the right horizon is an unnamed cone on the SW flank of Ostry, which erupted about 4,000 years ago producing a basaltic lava flow. · Foto: Copyrighted photo by Maria Pevzner, 2005 (Russian Academy of Sciences, Moscow). · Wikimedia Commons
Tipe
Stratovolkan
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
Ketinggian
2552 m
Koordinat
58.180, 160.820
Letusan terakhir
-2050
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

Conical Ostry volcano (also known as Ostraya) is a late-Quaternary stratovolcano on the western side of the major NE-trending graben along the axis of the northern Sredinny Range. An unnamed cinder cone on the SW flank, informally referred to as "Cone X," erupted about 4,000 years ago, producing a basaltic lava flow.

Ringkasan Wikipedia

Ringkasan Inggris

Ostry is a stratovolcano located in the northern part of the Kamchatka Peninsula, Russia. It comprises the higher Ostry volcano and the smaller Kutina volcano. Ostry is one of the highest peaks of Sredinny Range.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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2050 BCE~2050 BCE · 1 letusan · VEI maks. ?2050 BCE2050 BCE2049 BCE2049 BCE2049 BCE

Garis waktu rinci

  1. 2050 SMVEI ?Perkiraan geologi
    BCE 2050 – Berlangsung
    SW flank cinder cone

Tautan eksternal

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