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Želtovskij

Zheltovsky

Stratovulcano · Russia · 1926 m

Zheltovsky, seen here from Diky Greben volcano to its SW, was constructed during the last 8,000 years within a 4 x 5 km caldera truncating an earlier Pleistocene edifice. A late-Holocene explosive eruption formed a 1.6-km-wide summit crater that was largely filled by four lava domes, the latest of which forms the present summit. A large eruption in 1923 produced explosive activity and a lava flow down the SE flank that partially flowed into a crater.
Zheltovsky, seen here from Diky Greben volcano to its SW, was constructed during the last 8,000 years within a 4 x 5 km caldera truncating an earlier Pleistocene edifice. A late-Holocene explosive eruption formed a 1.6-km-wide summit crater that was largely filled by four lava domes, the latest of which forms the present summit. A large eruption in 1923 produced explosive activity and a lava flow down the SE flank that partially flowed into a crater. · Foto: Photo by Oleg Volynets (Institute of Volcanology, Petropavlovsk). · Wikimedia Commons
Tipo
Stratovulcano
Paese
Russia
Regione
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Altitudine
1926 m
Coordinate
51.577, 157.328
Ultima eruzione
1923
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

Zheltovsky volcano was constructed during the last 8000 years within a 4 x 5 km caldera truncating an earlier Pleistocene edifice. A late-Holocene explosive eruption formed a 1.6-km-wide summit crater that was subsequently largely filled by four lava domes, the latest of which forms the present summit. Several of the lava domes were emplaced along the buried SE rim of the summit crater. More than ten cinder cones and lava domes were constructed on the flanks, particularly on the NW side. Only a few eruptions are known in historical time. The largest, in 1923, produced explosive activity and a lava flow down the SE flank that also partly flowed into the summit crater.

Sintesi da Wikipedia

Lo Želtovskij è uno stratovulcano situato nella Kamčatka meridionale. Eruttò per l'ultima volta il 19 aprile 2018.

Wikipedia · CC BY-SA · Leggi l'articolo completo

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
7050 BCE~6749 BCE · 1 eruzioni · VEI max. 56148 BCE~5847 BCE · 1 eruzioni · VEI max. ?3140 BCE~2840 BCE · 1 eruzioni · VEI max. 51671~1972 · 3 eruzioni · VEI max. 37050 BCE4945 BCE2539 BCE434 BCE1671

Cronologia dettagliata

  1. 1972VEI 1Stima geologica
    1972-03-16 – In corso
  2. 1923VEI 3Osservata
    1923-02-11 – 1923-04
  3. 1823 (±5 anni)VEI ?Stima geologica
    1823 – In corso
  4. 3050 a.C.VEI 5Stima geologica
    BCE 3050 – In corso
  5. 6050 a.C.VEI ?Stima geologica
    BCE 6050 – In corso
  6. 7050 a.C. (±1000 anni)VEI 5Stima geologica
    BCE 7050 – In corso

Link esterni

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