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Chikurachki

Stratovolkan · Russia · 1781 m

The NW slopes of Chikurachki, the highest volcano on Paramushir Island, rises above the Sea of Okhotsk. Oxidized scoria covering the upper part of the cone result in the distinctive red color. The Tatarinov group of six volcanic centers is located immediately to the south of Chikurachki, forming the ridge to the right. In contrast to the frequently active Chikurachki, the Tatarinov volcanoes are extensively eroded and have a more complex structure.
The NW slopes of Chikurachki, the highest volcano on Paramushir Island, rises above the Sea of Okhotsk. Oxidized scoria covering the upper part of the cone result in the distinctive red color. The Tatarinov group of six volcanic centers is located immediately to the south of Chikurachki, forming the ridge to the right. In contrast to the frequently active Chikurachki, the Tatarinov volcanoes are extensively eroded and have a more complex structure. · Foto: Photo by Yoshihiro Ishizuka, 2000 (Hokkaido University). · Wikimedia Commons
Tipe
Stratovolkan
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Ketinggian
1781 m
Koordinat
50.324, 155.461
Letusan terakhir
2023
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

Chikurachki, the highest volcano on Paramushir Island in the northern Kuriles, is a relatively small cone constructed on a high Pleistocene edifice. Oxidized basaltic-to-andesitic scoria deposits covering the upper part of the cone give it a distinctive red color. Frequent basaltic Plinian eruptions have occurred during the Holocene. Lava flows have reached the sea and formed capes on the NW coast; several young lava flows are also present on the E flank beneath a scoria deposit. The Tatarinov group of six volcanic centers is located immediately to the south, and the Lomonosov cinder cone group, the source of an early Holocene lava flow that reached the saddle between it and Fuss Peak to the west, lies at the southern end of the N-S-trending Chikurachki-Tatarinov complex. The Tatarinov centers are extensively modified by erosion and have a more complex structure. Tephrochronology gives evidence of an eruption around 1690 CE from Tatarinov, although its southern cone contains a sulfur-encrusted crater with fumaroles that were active along the margin of a crater lake until 1959.

Ringkasan Wikipedia

Chikurachki adalah gunung berapi kerucut yang terletak di Pulau Paramushir, Kamchatka, Rusia. Gunung ini adalah gunung tertinggi di Pulau Paramushir. Chikurachki meletus pada tahun 2003, 2005,2007,2008,2016 dan 2022. Letusan terbaru terjadi pada 24 Juni 2022 di mana gunung ini mengeluarkan awan abu setinggi 5.000 meter.

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Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
9360 BCE~8981 BCE · 1 letusan · VEI maks. 28601 BCE~8222 BCE · 1 letusan · VEI maks. ?7842 BCE~7463 BCE · 1 letusan · VEI maks. 26325 BCE~5945 BCE · 1 letusan · VEI maks. 42151 BCE~1771 BCE · 1 letusan · VEI maks. 41771 BCE~1392 BCE · 2 letusan · VEI maks. 41644~2023 · 22 letusan · VEI maks. 49360 BCE6704 BCE3668 BCE1012 BCE1644

Garis waktu rinci

  1. 2023VEI 2Teramati
    2023-01-28 – 2023-02-08
  2. 2022VEI 2Teramati
    2022-01-17 – 2022-10-17
  3. 2021VEI 1Teramati
    2021-03-21 – 2021-08-25
  4. 2016VEI 2Teramati
    2016-07-27 – 2016-08-30
    Summit crater
  5. 2016VEI 2Teramati
    2016-03-29 – 2016-03-31
    Summit crater
  6. 2015VEI 3Teramati
    2015-02-16 – 2015-02-18
    Summit crater
  7. 2008VEI 2Teramati
    2008-07-29 – 2008-08-08
  8. 2007VEI 2Teramati
    2007-03-04 – 2007-04-18
  9. 2007VEI 2Teramati
    2007-08-19 – 2007-11-01
  10. 2005VEI 1Teramati
    2005-03-12 – 2005-04-07
  11. 2003VEI 2Teramati
    2003-04-17 – 2003-07-03
  12. 2002VEI 2Teramati
    2002-01-25 – 2002-04-22
    SSE part of summit crater
  13. 1986VEI 4Teramati
    1986-11-18 – 1986-12-07
  14. 1973VEI 2Teramati
    1973-08-10 – 1973-09-28
  15. 1967VEI 2Teramati
    1967-09-06 – 1967-09-20
  16. 1964VEI 2Teramati
    1964-02-01 – 1964-02-16
  17. 1961VEI 1Teramati
    1961-05-02 – 1961-08-10
  18. 1958VEI 2Teramati
    1958-05-26 – 1958-05-27
  19. 1957VEI 2Teramati
    1957-05-16 – Berlangsung
  20. 1933VEI ?Perkiraan geologi
    1933-04-15 – Berlangsung
  21. 1853VEI 3Teramati
    1853-12 – 1859
  22. 1690 (±10 tahun)VEI 4Perkiraan geologi
    1690 – Berlangsung
    Tatarinov
  23. 1500 SM (±250 tahun)VEI 4Perkiraan geologi
    BCE 1500 – Berlangsung
  24. 1750 SMVEI 3Perkiraan geologi
    BCE 1750 – Berlangsung
  25. 1950 SMVEI 4Perkiraan geologi
    BCE 1950 – Berlangsung
  26. 6310 SM (±70 tahun)VEI 4Perkiraan geologi
    BCE 6310 – Berlangsung
  27. 7550 SMVEI 2Perkiraan geologi
    BCE 7550 – Berlangsung
  28. 8500 SM (±950 tahun)VEI ?Perkiraan geologi
    BCE 8500 – Berlangsung
    Lomonosov
  29. 9360 SM (±80 tahun)VEI 2Perkiraan geologi
    BCE 9360 – Berlangsung

Tautan eksternal

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