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Chirpoy

Chirpoi

Caldera · Russia · 742 m

Chirpoi Island contains multiple volcanic edifices constructed within an 8-9 km wide, partially submerged caldera. This view from the east shows the Snow cone (left), Cherny (center), and the eroded Chirpoi to the right. Cherny erupted twice during the 18th and 19th centuries and Snow erupted between 1770 and 1810. It is composed almost entirely of lava flows, some of which form the shoreline in the foreground.
Chirpoi Island contains multiple volcanic edifices constructed within an 8-9 km wide, partially submerged caldera. This view from the east shows the Snow cone (left), Cherny (center), and the eroded Chirpoi to the right. Cherny erupted twice during the 18th and 19th centuries and Snow erupted between 1770 and 1810. It is composed almost entirely of lava flows, some of which form the shoreline in the foreground. · Foto: Photo by Oleg Volynets (Institute of Volcanology, Petropavlovsk). · Wikimedia Commons
Tipo
Caldera
Paese
Russia
Regione
Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
Altitudine
742 m
Coordinate
46.532, 150.871
Ultima eruzione
2016
Contesto tettonico
Subduction zone / Oceanic crust (< 15 km)
Forma vulcanica
Composite
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

Chirpoi, a small island lying between the larger islands of Simushir and Urup, contains a half dozen volcanic edifices constructed within an 8-9 km wide, partially submerged caldera. The southern rim of the caldera is exposed on nearby Brat Chirpoev Island. The symmetrical Cherny volcano, which forms the central cone of the island, erupted twice during the 18th and 19th centuries. The youngest volcano, Snow, originated between 1770 and 1810. It is composed almost entirely of lava flows, many of which have reached the sea on the southern coast. No recorded eruptions are known from Brat Chirpoev, but its youthful morphology suggests recent Strombolian activity.

Sintesi da Wikipedia

Riassunto in inglese

Chyornye Bratya is a pair of uninhabited volcanic islands between Simushir and Urup in the Kuril Islands chain in the Sea of Okhotsk in the northwest Pacific Ocean. The larger (northern) of the two is Chirpoy, and the smaller (southern) is Brat Chirpoyev. The origin of the names is uncertain: the original Ainu language name of the island was Repunmosir, a word meaning “place of many small birds”.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
1712~1742 · 1 eruzioni · VEI max. 41772~1802 · 1 eruzioni · VEI max. ?1802~1832 · 1 eruzioni · VEI max. 21832~1862 · 2 eruzioni · VEI max. 31862~1892 · 1 eruzioni · VEI max. 21952~1982 · 1 eruzioni · VEI max. 21982~2012 · 2 eruzioni · VEI max. 217121772186219221982

Cronologia dettagliata

  1. 2012VEI 0Osservata
    2012-11-11 – 2016-10-18
    Snow
  2. 1982VEI 2Osservata
    1982-11-22 – In corso
    Snow
  3. 1960VEI 2Osservata
    1960-10-20 – In corso
    Snow
  4. 1879VEI 2Osservata
    1879-05 – 1879-06
    Snow
  5. 1857VEI 3Osservata
    1857-07 – In corso
    Cherny
  6. 1854VEI 2Osservata
    1854-06-24 – In corso
    Snow (or Cherny)
  7. 1811VEI 2Osservata
    1811-06-11 – In corso
    Snow
  8. 1790 (±20 anni)VEI ?Osservata
    1790 – In corso
    Snow
  9. 1712VEI 4Osservata
    1712-12-31 – In corso
    Cherny

Link esterni

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