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Atlasov

Nylgimelkin

Gunung api perisai · Russia · 1764 m

This cone formed at the top of Nylgimelkin, with the larger Pleistocene Khuvkhoitun volcano visible in the background. Lava flows from Nylgimelkin were erupted along a fissure about 5,500 years ago.
This cone formed at the top of Nylgimelkin, with the larger Pleistocene Khuvkhoitun volcano visible in the background. Lava flows from Nylgimelkin were erupted along a fissure about 5,500 years ago. · Foto: Copyrighted photo by Maria Pevzner, 2005 (Russian Academy of Sciences, Moscow).
Tipe
Gunung api perisai
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
Ketinggian
1764 m
Koordinat
57.970, 160.650
Letusan terakhir
-3550
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Shield
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

The basaltic Nylgimelkin (also known as Atlasov) shield volcano and the topographically higher but smaller shield of Novagrablenova are dwarfed by their neighbor, the glacier-clad Pleistocene Khuvkhoitun, the highest Quaternary volcano of the northern Sredinny Range. The two youthful shields were constructed on the W and NW flanks of Khuvkhoitun. Lava flows from them extend primarily to the west. Cinder cones and a lava flow were erupted along a fissure at Nylgimelkin about 5,500 years ago.

Ringkasan Wikipedia

Ringkasan Inggris

Atlasova is a basaltic shield volcano situated in Kamchatka. It is named after Russian explorer Vladimir Atlasov.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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3550 BCE~3550 BCE · 1 letusan · VEI maks. ?3550 BCE3550 BCE3549 BCE3549 BCE3549 BCE

Garis waktu rinci

  1. 3550 SMVEI ?Perkiraan geologi
    BCE 3550 – Berlangsung

Tautan eksternal

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