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Rusia · Gunung api perisai

Titila

Tipe: Gunung api perisai
Ketinggian: 1523 m
Letusan terakhir: -550

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: Rusia
Wilayah: Pasifik Barat Laut / Central Kamchatka Volcanic Arc
Ketinggian: 1523 m
Koordinat: 57.406, 160.108
Letusan terakhir: -550
Kondisi tektonik: Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan: Perisai
Batuan utama: Basal / Pikrobasal

Ringkasan geologi

Teks asli bahasa Inggris

Titila is a small basaltic shield volcano NW of Lake Glubokoye, west of the crest of the central Sredinny Range.

Kutipan dari Global Volcanism Program, Smithsonian Institution · Baca ringkasan lengkap di GVP →

Ringkasan Wikipedia

Ringkasan Inggris

Titila is a shield volcano located in the northern part of Kamchatka Peninsula, Russia.

Wikipedia · CC BY-SA · Lanjutkan membaca di Wikipedia bahasa Inggris →

Riwayat letusan

1 tercatatGlosarium

Ringkasan catatan

Letusan terkonfirmasi: 1
Letusan tidak pasti: 0
Rentang catatan terkonfirmasi: 550 SM – 550 SM
Letusan terkonfirmasi terbesar: Tidak ada VEI tercatat
Letusan terkonfirmasi sejak 1900: 0

Ringkasan (VEI dari waktu ke waktu)

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Garis waktu rinci

550 SMVEI ?Perkiraan geologi
550 SM – akhir tidak diketahui

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