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Titila

Gunung api perisai · Russia · 1523 m

Titila volcano is viewed looking towards the SE. It started to erupt in the late Pleistocene and was active about 10,000-8,000 and 3,000-2,500 years ago. A flank vent (forming the peak to the right) formed during the early Holocene. Its lava flows dammed a river to form Glubokoye Lake to the right.
Titila volcano is viewed looking towards the SE. It started to erupt in the late Pleistocene and was active about 10,000-8,000 and 3,000-2,500 years ago. A flank vent (forming the peak to the right) formed during the early Holocene. Its lava flows dammed a river to form Glubokoye Lake to the right. · Foto: Copyrighted photo by Maxim Portnyagin (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
Tipe
Gunung api perisai
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
Ketinggian
1523 m
Koordinat
57.406, 160.108
Letusan terakhir
-550
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Shield
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

Titila is a small basaltic shield volcano NW of Lake Glubokoye, west of the crest of the central Sredinny Range. Lava flows radiate from two summit craters, and cinder cones are prominent on its southern flank. Titila overlaps to the W with another small shield volcano, Rassoshina, along with other features in the Sedanka Lava Field to the south. The latest known eruption took place about 2,500 years ago.

Ringkasan Wikipedia

Ringkasan Inggris

Titila is a shield volcano located in the northern part of Kamchatka Peninsula, Russia. It comprises two shield volcanoes: Titila and Rassoshina, from which Titila is the higher one.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
550 BCE~550 BCE · 1 letusan · VEI maks. ?550 BCE550 BCE549 BCE549 BCE549 BCE

Garis waktu rinci

  1. 550 SMVEI ?Perkiraan geologi
    BCE 550 – Berlangsung

Tautan eksternal

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