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Parícutin

Michoacan-Guanajuato

Campo vulcanico · Mexico · 3860 m

Parícutin, the volcano that grew in a cornfield in 1943, is a well-known feature of the Michoacán-Guanajuato volcanic field. The huge field contains over 1,400 vents covering a wide area across the Michoacán and Guanajuato states. Scoria cones are the predominant volcanic landform, and lava domes, maars, tuff rings, and lava flows are also present. Parícutin is seen here from the NE with the Nueva Juatita flank vent in the foreground, the main source of lava during the last five years of the eruption.
Parícutin, the volcano that grew in a cornfield in 1943, is a well-known feature of the Michoacán-Guanajuato volcanic field. The huge field contains over 1,400 vents covering a wide area across the Michoacán and Guanajuato states. Scoria cones are the predominant volcanic landform, and lava domes, maars, tuff rings, and lava flows are also present. Parícutin is seen here from the NE with the Nueva Juatita flank vent in the foreground, the main source of lava during the last five years of the eruption. · Foto: Photo by Jim Luhr, 1997 (Smithsonian Institution). · Wikimedia Commons
Tipo
Campo vulcanico
Paese
Mexico
Regione
Middle America-Caribbean Volcanic Regions / Trans-Mexican Volcanic Arc
Altitudine
3860 m
Coordinate
19.850, -101.750
Ultima eruzione
1952
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Cluster
Roccia principale
Andesite / Basaltic Andesite
Sintesi geologica

The widespread Michoacán-Guanajuato volcanic field contains over 1,400 vents, including the historically active cinder cones of Parícutin and Jorullo, covering a 200 x 250 km wide area of Michoacán and Guanajuato states in west-central México. Cinder cones are the predominant volcanic form, but small shield volcanoes, lava domes, maars and tuff rings (many in the Valle de Santiago area), and coneless lava flows are also present. The volcanoes with shield-type morphologies are mostly Pleistocene in age, although the Michoacán-Guanajuato centers have higher slope angles and smaller basal diameters. Jorullo, which was constructed in the 18th century, and Parícutin, which grew above a former cornfield during 1943-52, are the two best known volcanic features scattered throughout the field.

Sintesi da Wikipedia

Il vulcano Paricutín o Parícutin è il vulcano più giovane al mondo e appare in alcune versioni delle Sette Meraviglie Naturali del Mondo. Si trova nello Stato di Michoacán, in Messico tra il villaggio di San Juan Parangaricutiro e quello di Angahuan. Ha preso il nome dal villaggio omonimo che rimase completamente sommerso dalla sua eruzione iniziata il 20 febbraio del 1943.

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
7350 BCE~7040 BCE · 1 eruzioni · VEI max. 36730 BCE~6421 BCE · 1 eruzioni · VEI max. 36111 BCE~5801 BCE · 1 eruzioni · VEI max. ?4252 BCE~3943 BCE · 1 eruzioni · VEI max. ?3013 BCE~2703 BCE · 1 eruzioni · VEI max. 32084 BCE~1774 BCE · 2 eruzioni · VEI max. 31155 BCE~845 BCE · 1 eruzioni · VEI max. ?1014~1323 · 1 eruzioni · VEI max. ?1633~1943 · 2 eruzioni · VEI max. 47350 BCE5182 BCE2703 BCE535 BCE1633

Cronologia dettagliata

  1. 1943VEI 4Osservata
    1943-02-20 – 1952-02-25
    Parícutin
  2. 1759VEI 4Osservata
    1759-09-29 – 1774
    Jorullo
  3. 1050 (±50 anni)VEI ?Stima geologica
    1050 – In corso
    Valle de Santiago
  4. 1140 a.C. (±865 anni)VEI ?Stima geologica
    BCE 1140 – In corso
    Cerro el Zoyate
  5. 1880 a.C. (±150 anni)VEI 3Stima geologica
    BCE 1880 – In corso
    Cerro el Jabalí
  6. 2050 a.C.VEI ?Stima geologica
    BCE 2050 – In corso
    Valle de Santiago (La Alberca)
  7. 2750 a.C. (±200 anni)VEI 3Stima geologica
    BCE 2750 – In corso
    Cerro el Metate
  8. 4140 a.C. (±300 anni)VEI ?Stima geologica
    BCE 4140 – In corso
    Cerro la Tinaja
  9. 5940 a.C. (±335 anni)VEI ?Stima geologica
    BCE 5940 – In corso
    Cerro Grande?
  10. 6480 a.C. (±300 anni)VEI 3Stima geologica
    BCE 6480 – In corso
    Cerro la Taza
  11. 7350 a.C. (±300 anni)VEI 3Stima geologica
    BCE 7350 – In corso
    Hoyo el Huanillo

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⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.