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Kikhpinych

Stratovolcano · Russia · 1515m

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. · Photo: Copyrighted photo by Vera Ponomareva (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm). · Wikimedia Commons
Type
Stratovolcano
Country
Russia
Region
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Elevation
1515m
Coordinates
54.489, 160.251
Last eruption
1550
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Basalt / Picro-Basalt
Geological summary

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.

From Wikipedia

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

Wikipedia · CC BY-SA · Read full article

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
2850 BCE~2650 BCE · 2 eruptions · max VEI 4550~750 · 2 eruptions · max VEI 3750~950 · 2 eruptions · max VEI 31350~1550 · 2 eruptions · max VEI 42850 BCE1850 BCE650 BCE3501350

Detailed timeline

  1. 1550VEI ?Geological estimate
    1550 – Ongoing
    East flank of Savich (Krab cone)
  2. 1350VEI 4Geological estimate
    1350 – Ongoing
    Savich cone and north flank
  3. 900 (±50 yrs)VEI 3Geological estimate
    900 – Ongoing
    Savich cone
  4. 830 (±25 yrs)VEI ?Geological estimate
    830 – Ongoing
    Savich cone
  5. 650VEI ?Geological estimate
    650 – Ongoing
    Savich cone
  6. 550VEI 3Geological estimate
    550 – Ongoing
    East side of Zapadny, Savich cone
  7. 2780 BCE (±25 yrs)VEI 4Geological estimate
    BCE 2780 – Ongoing
    Zapadny
  8. 2850 BCEVEI 3Geological estimate
    BCE 2850 – Ongoing
    Zapadny

External links

⚠ For reference only. Not for emergency response.