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Khangar

Stratovolkan · Russia · 1967 m

Khangar is the southernmost volcano of the N-S-trending Sredinny Range, which stretches across western Kamchatka. It contains a 2.8-km-wide summit crater and a large lava dome on its eastern flank. The crater formed about 7,000 years ago and is now partially filled by a lake.
Khangar is the southernmost volcano of the N-S-trending Sredinny Range, which stretches across western Kamchatka. It contains a 2.8-km-wide summit crater and a large lava dome on its eastern flank. The crater formed about 7,000 years ago and is now partially filled by a lake. · Foto: Photo by Dan Miller, 1990 (U.S. Geological Survey). · Wikimedia Commons
Tipe
Stratovolkan
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
Ketinggian
1967 m
Koordinat
54.761, 157.407
Letusan terakhir
1500
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Dacite
Ringkasan geologi

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.

Ringkasan Wikipedia

Ringkasan Inggris

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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9500 BCE~9133 BCE · 1 letusan · VEI maks. 48400 BCE~8033 BCE · 1 letusan · VEI maks. ?7300 BCE~6933 BCE · 1 letusan · VEI maks. ?6567 BCE~6200 BCE · 1 letusan · VEI maks. ?5833 BCE~5467 BCE · 2 letusan · VEI maks. 62900 BCE~2533 BCE · 1 letusan · VEI maks. ?700 BCE~333 BCE · 1 letusan · VEI maks. ?767~1133 · 1 letusan · VEI maks. ?1133~1500 · 1 letusan · VEI maks. ?9500 BCE6933 BCE4000 BCE1433 BCE1133

Garis waktu rinci

  1. 1500 (±40 tahun)VEI ?Perkiraan geologi
    1500 – Berlangsung
  2. 1000 (±16 tahun)VEI ?Perkiraan geologi
    1000 – Berlangsung
  3. 350 SM (±30 tahun)VEI ?Perkiraan geologi
    BCE 350 – Berlangsung
  4. 2700 SM (±25 tahun)VEI ?Perkiraan geologi
    BCE 2700 – Berlangsung
  5. 5500 SM (±25 tahun)VEI ?Perkiraan geologi
    BCE 5500 – Berlangsung
  6. 5700 SM (±16 tahun)VEI 6Perkiraan geologi
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  7. 6400 SM (±75 tahun)VEI ?Perkiraan geologi
    BCE 6400 – Berlangsung
  8. 7100 SM (±100 tahun)VEI ?Perkiraan geologi
    BCE 7100 – Berlangsung
  9. 8250 SM (±100 tahun)VEI ?Perkiraan geologi
    BCE 8250 – Berlangsung
  10. 9500 SM (±300 tahun)VEI 4Perkiraan geologi
    BCE 9500 – Berlangsung

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