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Atlasov

Nylgimelkin

Tipe
Gunung api perisai
Ketinggian
1764 m
Letusan terakhir
-3550
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
Rusia
Wilayah
Pasifik Barat Laut / Central Kamchatka Volcanic Arc
Ketinggian
1764 m
Koordinat
57.970, 160.650
Letusan terakhir
-3550
Kondisi tektonik
Zona subduksi / Kerak benua (> 25 km)
Bentuk lahan
Perisai
Batuan utama
Basal / Pikrobasal
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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3550 SM~3550 SM · 1 letusan · VEI maks. ?3550 SM3550 SM3549 SM3549 SM3549 SM

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  1. 3550 SMVEI ?Perkiraan geologi
    3550 SM – akhir tidak diketahui

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