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Gorny Institute

Stratovolkan · Russia · 2125 m

Gorny Institute volcano, seen here from the south, lies at the NE end of chain of small late-Quaternary volcanoes extending NE from Kebeney volcano in the central Sredinny Range. It is one of the large stratovolcanoes in the Sredinny Range that have been active during the Holocene.
Gorny Institute volcano, seen here from the south, lies at the NE end of chain of small late-Quaternary volcanoes extending NE from Kebeney volcano in the central Sredinny Range. It is one of the large stratovolcanoes in the Sredinny Range that have been active during the Holocene. · Foto: Copyrighted photo by Maria Pevzner, 2004 (Russian Academy of Sciences, Moscow).
Tipe
Stratovolkan
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
Ketinggian
2125 m
Koordinat
57.330, 160.200
Letusan terakhir
1250
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

Gorny Institute volcano lies at the NE end of chain of small late-Quaternary volcanoes extending NE from Kebeney volcano in the central Sredinny Range. It was constructed near the steep-walled eastern margin of a major NE-SW-trending graben extending NE from Kebeney volcano. A line of cinder cones with the same orientation is located on the NE and SW flanks. More than 20 pyroclastic horizons have been documented, and the last major eruption took place about 700 years ago.

Ringkasan Wikipedia

Ringkasan Inggris

Gorny Institute, also spelled Gornyi Institut, is a stratovolcano located in the Sredinny Range on Russia's Kamchatka Peninsula. It lies just east of the Titila volcano and north of the Kebeney volcano.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
4250 BCE~4054 BCE · 1 letusan · VEI maks. 0857~1054 · 1 letusan · VEI maks. ?1054~1250 · 1 letusan · VEI maks. ?4250 BCE2875 BCE1500 BCE321 BCE1054

Garis waktu rinci

  1. 1250VEI ?Perkiraan geologi
    1250 – Berlangsung
  2. 1000VEI ?Perkiraan geologi
    1000 – Berlangsung
  3. 4250 SMVEI 0Perkiraan geologi
    BCE 4250 – Berlangsung
    South flank (Sedanka lava flow)

Tautan eksternal

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