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Rusia · Stratovolkan

Uratman

Tipe
Stratovolkan
Ketinggian
678 m
Letusan terakhir
Tidak diketahui
Uratman
Public domain · Wikimedia Commons
Tipe
Stratovolkan
Negara
Rusia
Wilayah
Pasifik Barat Laut / Kuril Volcanic Arc
Ketinggian
678 m
Koordinat
47.120, 152.250
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona subduksi / Kerak samudra (< 15 km)
Bentuk lahan
Komposit
Batuan utama
Andesit / Andesit basaltik
Ringkasan geologi

The northernmost volcano on Simushir Island, Uratman consists of a 7.5-km-wide Pleistocene caldera with walls that rise 450 m above a 250-m-deep caldera bay. A narrow gap in the northern rim provides ocean access into Brouton Bay, which fills the NW half of the caldera. The andesitic central cone grew during the Holocene in the SE part of the caldera. Two cinder cones are located along the N flank of Uratman, and a lava dome was formed on its NW flank along Brouton Bay. No recorded eruptions are known.

Ringkasan Wikipedia

Ringkasan Inggris

Uratman is a somma volcano located at the northern end of Simushir Island, Kuril Islands, Russia. It consists of a Pleistocene caldera which contains an andesite cone of Holocene age. The caldera is exposed to the ocean, forming Brouton Bay.

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