Khangar
Stratovolcano · Russia · 1967m

- Type
- Stratovolcano
- Country
- Russia
- Region
- Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
- Elevation
- 1967m
- Coordinates
- 54.761, 157.407
- Last eruption
- 1500
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Dacite
Geological summary
Khangar volcano, also spelled Hangar, is the southernmost volcano of the Sredinny Range, which stretches N-S across western Kamchaktka. It is the dominant feature within a larger volcano-tectonic depression composed of two parts: a stratovolcano with a 2-km-wide Holocene caldera, and a large lava dome on its eastern flank. The steep-walled caldera, now filled by a lake, was formed during a major explosive eruption about 7,000 years ago. An arcuate zone of pre-caldera flank lava domes nearly surrounds the volcano, and post-caldera domes form islands in the caldera lake. Late-stage olivine basalts were erupted along a NE-trending line in the southern part of the depression. The latest dated eruption took place about 500 years ago.
From Wikipedia
Khangar is a stratovolcano located in the central part of Kamchatka Peninsula, Russia. It is the southernmost volcano of the Sredinny Range. Its 2 km-wide caldera is now filled by a lake.
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Eruption history
Detailed timeline
- 1500 (±40 yrs)VEI ?Geological estimate1500 – Ongoing
- 1000 (±16 yrs)VEI ?Geological estimate1000 – Ongoing
- 350 BCE (±30 yrs)VEI ?Geological estimateBCE 350 – Ongoing
- 2700 BCE (±25 yrs)VEI ?Geological estimateBCE 2700 – Ongoing
- 5500 BCE (±25 yrs)VEI ?Geological estimateBCE 5500 – Ongoing
- 5700 BCE (±16 yrs)VEI 6Geological estimateBCE 5700 – Ongoing
- 6400 BCE (±75 yrs)VEI ?Geological estimateBCE 6400 – Ongoing
- 7100 BCE (±100 yrs)VEI ?Geological estimateBCE 7100 – Ongoing
- 8250 BCE (±100 yrs)VEI ?Geological estimateBCE 8250 – Ongoing
- 9500 BCE (±300 yrs)VEI 4Geological estimateBCE 9500 – Ongoing
External links
⚠ For reference only. Not for emergency response.