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Cherpuk Group

Kerucut piroklastik · Russia · 1868 m

The Yuzhny Cherpuk cinder cone (left-center horizon) and its andesitic lava flow are located 11 km SSW from Ichinsky volcano. The fresh-looking lava flow was erupted about 6,500 years ago and traveled 18 km. Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that was constructed along the crest of the Sredinny Range.
The Yuzhny Cherpuk cinder cone (left-center horizon) and its andesitic lava flow are located 11 km SSW from Ichinsky volcano. The fresh-looking lava flow was erupted about 6,500 years ago and traveled 18 km. Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that was constructed along the crest of the Sredinny Range. · Foto: Copyrighted photo by Adam Kirilenko, 2000 (Holocene Kamchatka Volcanoes, www.kamchatka.ginras.ru).
Tipe
Kerucut piroklastik
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
Ketinggian
1868 m
Koordinat
55.550, 157.470
Letusan terakhir
-4550
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Minor
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

Severny Cherpuk (South Cherpuk) and Yuzhny Cherpuk (North Cherpuk) are two cinder cones SW of Ichinsky volcano that comprise the largest monogenetic volcanoes of the Sredinny Range. Severny Cherpuk, 21 km SW of Ichinsky, is a double cone that fed 1.8 km3 lava flows down both sides of the range to the NW and SE. A narrow tongue of the SE flow diverted an additional 10 km S, for a total distance of 22 km. Yuzhny Cherpuk, 11 km SSW of Ichinsky, produced a 1.7 km3 lava flow that traveled 18 km S and then SE. The flow descended to 640 m elevation and dammed tributaries of the Ketachan River, producing three lakes. The two cones are sometimes considered to be satellitic cones to Ichinsky, but Pevzner et al. (2000) noted petrological distinctions that suggest an independent origin. Unpublished radiocarbon ages revise those in Pevzner et al. (2000) and indicate that both cones were formed about 6,500 years ago.

Ringkasan Wikipedia

Ringkasan Inggris

Cherpuk Group is a group of two cinder cones located in the central part of Kamchatka Peninsula, Russia. It is a group of a few mostly dormant cinder cones.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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4550 BCE~4550 BCE · 1 letusan · VEI maks. ?4550 BCE4550 BCE4549 BCE4549 BCE4549 BCE

Garis waktu rinci

  1. 4550 SMVEI ?Perkiraan geologi
    BCE 4550 – Berlangsung
    North and South Cherpuk

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