Kizimen
Stratovolcano in Russia
Key Facts
Elevation
2,334 m (7,657 ft)
Type
Stratovolcano
Location
55.131°, 160.320°
Region
Eastern Kamchatka Volcanic Arc
Rock Type
Andesite / Basaltic Andesite
Tectonic Setting
Subduction zone
Location
Loading map...
Overview
Kizimen is an isolated, conical stratovolcano that is morphologically similar to St. Helens prior to its 1980 eruption. The summit consists of overlapping lava domes, and blocky lava flows descend the flanks of the volcano, which is the westernmost of a volcanic chain north of Kronotsky volcano.
The 2334-m-high edifice was formed during four eruptive cycles beginning about 12,000 years ago and lasting 2000-3500 years. The largest eruptions took place about 10,000 and 8300-8400 years ago, and three periods of long-term lava dome growth have occurred. The latest eruptive cycle began about 3000 years ago with a large explosion and was followed by intermittent lava dome growth lasting about 1000 years.
An explosive eruption about 1100 years ago produced a lateral blast and created a 1. 0 x 0. 7 km wide crater breached to the NE, inside which a small lava dome (the fourth at Kizimen) has grown.
Prior to 2010, only a single explosive eruption, during 1927-28, had been recorded in historical time.
Volcanic Hazards & Risk Assessment
Primary Hazards
- Pyroclastic flows
- Lava flows
- Volcanic bombs and ballistics
- Lahars and mudflows
Risk Level
Geological Composition & Structure
Rock Types
Tectonic Setting
Age & Formation
Eruption Statistics & Analysis
| Metric | Value | Global Ranking | Significance |
|---|---|---|---|
| Total Recorded Eruptions | Unknown | Low | Moderately active volcano |
| Maximum VEI | VEI Unknown | Minor | Local impact potential |
| Recent Activity | 13 years ago | Recent | Recently active |
Monitoring & Alert Status
Monitoring Networks
Current Status
Nearby Volcanoes in Northwestern Pacific Volcanic Regions
Quick Info
- •Smithsonian ID: 300230
- •Evidence: Eruption Observed
- •Epoch: Holocene
About the Photo
Kizimen is seen here from the NW. The Holocene edifice is composed of closely spaced lava domes, lava flows, and pyroclastic-flow deposits. A faint plume from fumaroles are seen on the northern slope near the summit.
Copyrighted photo by Vikto Dvigalo (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
Authority Sources
Related Volcanoes
Basic Information
This page shows basic data from the Smithsonian Global Volcanism Program. For more detailed information, visit the official Smithsonian page.