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Terpuk

Gunung api perisai · Russia · 765 m

The northern (right) and southern (left) summits of the Terpuk edifice are viewed here from the ESE. Both cones formed about 3,000-2,500 years ago and produced an extensive lava field. The large green vegetated patch on the foreground is a Pleistocene lava flow surrounded by the Terpuk lava flows.
The northern (right) and southern (left) summits of the Terpuk edifice are viewed here from the ESE. Both cones formed about 3,000-2,500 years ago and produced an extensive lava field. The large green vegetated patch on the foreground is a Pleistocene lava flow surrounded by the Terpuk lava flows. · Foto: Copyrighted photo by Maxim Portnyagin (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm). · Wikimedia Commons
Tipe
Gunung api perisai
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
Ketinggian
765 m
Koordinat
57.200, 159.830
Letusan terakhir
-800
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Shield
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

Terpuk is a small basaltic shield volcano west of the crest of the Sredinny Range, south of Leutongey volcano, and NW of Kebeney volcano. The shield is topped by small cinder cones aligned NE-SW. Sparsely vegetated lava flows that radiate from the summit vents blocked local drainages, forming several small lakes. Topography constrains the flows to be longer toward the west, away from the crest of the range. The flows are among the youngest in the Sedankinsky Dol region and were erupted about 2,500-3,000 years ago.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
800 BCE~800 BCE · 1 letusan · VEI maks. ?800 BCE800 BCE799 BCE799 BCE799 BCE

Garis waktu rinci

  1. 800 SM (±300 tahun)VEI ?Perkiraan geologi
    BCE 800 – Berlangsung

Tautan eksternal

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