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Kikhpinych

Stratovulcano · Russia · 1515 m

Three Holocene cones of Kikhpinych are seen in this view from the west with the Pacific Ocean in the background. The distinct brown feature in the center is the Krab lava dome that grew on the E flank of Savich (back center), the youngest cone of the complex at about 1,400 years old. The peak at right is the mid-Holocene Zapadny cone. In the foreground is the Duga cone, which erupted about 3,200 years ago and produced lava flows up to 10 km long.
Three Holocene cones of Kikhpinych are seen in this view from the west with the Pacific Ocean in the background. The distinct brown feature in the center is the Krab lava dome that grew on the E flank of Savich (back center), the youngest cone of the complex at about 1,400 years old. The peak at right is the mid-Holocene Zapadny cone. In the foreground is the Duga cone, which erupted about 3,200 years ago and produced lava flows up to 10 km long. · Foto: Copyrighted photo by Vera Ponomareva (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Russia
Regione
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Altitudine
1515 m
Coordinate
54.489, 160.251
Ultima eruzione
1550
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

Kikhpinych, the youngest stratovolcano of the Eastern Volcanic Zone of Kamchatka, contains three summits constructed along a roughly E-W line above the eroded Pleistocene Pik volcano, NE of the Uzon caldera. Growth of the modern volcano began during the mid-Holocene about 4,800 years ago with construction of the Zapadny cone. After a long quiescence, the younger Savich cone was built about 1,400 years ago, which included strong explosive activity that destroyed part of the Zapadny and Pik cones. Numerous young lava flows mantle the flanks of Savich; it was last active about 400 years ago, when the Krab lava dome grew on its E flank. Numerous thermal fields are found throughout the complex, including two geysers (now the site of vigorous fumaroles) that were active in the summit crater of Stary Kikhpinych prior to burial by a rockfall avalanche that occurred sometime between September 1981 and July 1982.

Sintesi da Wikipedia

Riassunto in inglese

Kikhpinych is a stratovolcano located in the eastern part of the Kamchatka Peninsula, which feeds the famous Valley of Geysers.

Wikipedia · CC BY-SA · Leggi l'articolo completo

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
2850 BCE~2650 BCE · 2 eruzioni · VEI max. 4550~750 · 2 eruzioni · VEI max. 3750~950 · 2 eruzioni · VEI max. 31350~1550 · 2 eruzioni · VEI max. 42850 BCE1850 BCE650 BCE3501350

Cronologia dettagliata

  1. 1550VEI ?Stima geologica
    1550 – In corso
    East flank of Savich (Krab cone)
  2. 1350VEI 4Stima geologica
    1350 – In corso
    Savich cone and north flank
  3. 900 (±50 anni)VEI 3Stima geologica
    900 – In corso
    Savich cone
  4. 830 (±25 anni)VEI ?Stima geologica
    830 – In corso
    Savich cone
  5. 650VEI ?Stima geologica
    650 – In corso
    Savich cone
  6. 550VEI 3Stima geologica
    550 – In corso
    East side of Zapadny, Savich cone
  7. 2780 a.C. (±25 anni)VEI 4Stima geologica
    BCE 2780 – In corso
    Zapadny
  8. 2850 a.C.VEI 3Stima geologica
    BCE 2850 – In corso
    Zapadny

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.