Lewati ke konten utama
← Kembali ke peta
⇄ Bandingkan

Zhupanovsky

Gunung api majemuk · Russia · 2899 m

All four cones forming the WNW-trending Zhupanovsky massif are seen in this view from the west. The upper peak forms the summit of the complex. Steam plumes rise from the historically active crater in the center of the only Holocene cone; known eruptions have consisted of relatively minor explosions.
All four cones forming the WNW-trending Zhupanovsky massif are seen in this view from the west. The upper peak forms the summit of the complex. Steam plumes rise from the historically active crater in the center of the only Holocene cone; known eruptions have consisted of relatively minor explosions. · Foto: Photo by Oleg Volynets (Institute of Volcanology, Petropavlovsk). · Wikimedia Commons
Tipe
Gunung api majemuk
Negara
Russia
Wilayah
Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
Ketinggian
2899 m
Koordinat
53.589, 159.150
Letusan terakhir
2016
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Andesite / Basaltic Andesite
Ringkasan geologi

The Zhupanovsky volcanic massif consists of four overlapping stratovolcanoes along a WNW-trending ridge. The elongated complex was constructed within a Pliocene-early Pleistocene caldera whose rim is exposed only on the eastern side. Three of the stratovolcanoes were built during the Pleistocene. An early Holocene stage of frequent moderate and weak eruptions from 7,000 to 5,000 years before present (BP) was followed by a period of infrequent larger eruptions that produced pyroclastic flows. The last major eruption took place about 800-900 BP. Recorded eruptions have consisted of relatively minor explosions from Priemysh, the third cone from the E about 2.5 km from the summit peak.

Ringkasan Wikipedia

Ringkasan Inggris

Zhupanovsky is a volcanic massif located in the southeastern part of the Kamchatka Peninsula, Russia. It consists of four overlapping stratovolcanoes. After 54 years of inactivity, the volcano began erupting on 23 October 2013 and again in 2014, continuing nonstop into 2016.

Wikipedia · CC BY-SA · Baca artikel lengkap →

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
Klik pada bar untuk melihat letusan individu
5050 BCE~4814 BCE · 1 letusan · VEI maks. ?3166 BCE~2930 BCE · 1 letusan · VEI maks. ?339 BCE~104 BCE · 1 letusan · VEI maks. ?104 BCE~132 · 1 letusan · VEI maks. ?838~1074 · 1 letusan · VEI maks. ?1545~1780 · 1 letusan · VEI maks. 21780~2016 · 10 letusan · VEI maks. 35050 BCE3401 BCE1517 BCE1321780

Garis waktu rinci

  1. 2016VEI 2Teramati
    2016-11-20 – 2016-11-20
    Priemysh Crater
  2. 2015VEI 3Teramati
    2015-11-28 – 2016-03-25
    Priemysh Crater
  3. 2014VEI 3Teramati
    2014-06-06 – 2015-08-06
    Priemysh Crater
  4. 2013VEI 2Teramati
    2013-10-23 – 2013-10-26
    Summit crater
  5. 1959VEI 2Teramati
    1959-07-02 – Berlangsung
  6. 1956VEI 2Teramati
    1956-12-27 – 1957-06-16
    Middle crater, east crater
  7. 1940VEI 2Teramati
    1940-01 – 1940-02
  8. 1929VEI 2Teramati
    1929 – Berlangsung
  9. 1925VEI 2Teramati
    1925 – Berlangsung
  10. 1882VEI 2Teramati
    1882 – Berlangsung
  11. 1776VEI 2Teramati
    1776-10 – Berlangsung
  12. 1000 (±500 tahun)VEI ?Perkiraan geologi
    1000 – Berlangsung
  13. 50 SMVEI ?Perkiraan geologi
    BCE 50 – Berlangsung
  14. 220 SM (±50 tahun)VEI ?Perkiraan geologi
    BCE 220 – Berlangsung
  15. 3050 SMVEI ?Perkiraan geologi
    BCE 3050 – Berlangsung
  16. 5050 SMVEI ?Perkiraan geologi
    BCE 5050 – Berlangsung

Tautan eksternal

⚠ Untuk referensi saja. Bukan untuk tanggap darurat.