Čikurački
Chikurachki
Stratovulcano · Russia · 1781 m
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- Tipo
- Stratovulcano
- Paese
- Russia
- Regione
- Northwestern Pacific Volcanic Regions / Kuril Volcanic Arc
- Altitudine
- 1781 m
- Coordinate
- 50.324, 155.461
- Ultima eruzione
- 2023
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Basalt / Picro-Basalt
Sintesi geologica
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.
Sintesi da Wikipedia
Riassunto in ingleseChikurachki is the highest volcano on Paramushir Island in the northern Kuril Islands. It is actually a relatively small volcanic cone constructed on a high Pleistocene volcanic edifice. Oxidized andesitic scoria deposits covering the upper part of the young cone give it a distinctive red color. Lava flows from the 1,816-metre (5,958 ft) high Chikurachki reached the sea and formed capes on the northwest coast; several young lava flows also emerge from beneath the scoria blanket on the eastern flank.
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Storia delle eruzioni
Cronologia dettagliata
- 2023VEI 2Osservata2023-01-28 – 2023-02-08
- 2022VEI 2Osservata2022-01-17 – 2022-10-17
- 2021VEI 1Osservata2021-03-21 – 2021-08-25
- 2016VEI 2Osservata2016-07-27 – 2016-08-30Summit crater
- 2016VEI 2Osservata2016-03-29 – 2016-03-31Summit crater
- 2015VEI 3Osservata2015-02-16 – 2015-02-18Summit crater
- 2008VEI 2Osservata2008-07-29 – 2008-08-08
- 2007VEI 2Osservata2007-03-04 – 2007-04-18
- 2007VEI 2Osservata2007-08-19 – 2007-11-01
- 2005VEI 1Osservata2005-03-12 – 2005-04-07
- 2003VEI 2Osservata2003-04-17 – 2003-07-03
- 2002VEI 2Osservata2002-01-25 – 2002-04-22SSE part of summit crater
- 1986VEI 4Osservata1986-11-18 – 1986-12-07
- 1973VEI 2Osservata1973-08-10 – 1973-09-28
- 1967VEI 2Osservata1967-09-06 – 1967-09-20
- 1964VEI 2Osservata1964-02-01 – 1964-02-16
- 1961VEI 1Osservata1961-05-02 – 1961-08-10
- 1958VEI 2Osservata1958-05-26 – 1958-05-27
- 1957VEI 2Osservata1957-05-16 – In corso
- 1933VEI ?Stima geologica1933-04-15 – In corso
- 1853VEI 3Osservata1853-12 – 1859
- 1690 (±10 anni)VEI 4Stima geologica1690 – In corsoTatarinov
- 1500 a.C. (±250 anni)VEI 4Stima geologicaBCE 1500 – In corso
- 1750 a.C.VEI 3Stima geologicaBCE 1750 – In corso
- 1950 a.C.VEI 4Stima geologicaBCE 1950 – In corso
- 6310 a.C. (±70 anni)VEI 4Stima geologicaBCE 6310 – In corso
- 7550 a.C.VEI 2Stima geologicaBCE 7550 – In corso
- 8500 a.C. (±950 anni)VEI ?Stima geologicaBCE 8500 – In corsoLomonosov
- 9360 a.C. (±80 anni)VEI 2Stima geologicaBCE 9360 – In corso
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.