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Parícutin (or Volcán de Parícutin, also accented Paricutín) is a cinder cone volcano located in the Mexican state of Michoacán, near the city of Uruapan and about 322 kilometers (200 mi) west of Mexico City. The volcano surged suddenly from the cornfield of local farmer Dionisio Pulido in 1943, attracting both popular and scientific attention.
The city is called Nuevo (Spanish for "new") because the original San Juan Parangaricutiro was destroyed during the formation of the Parícutin volcano in 1943. [1] Along with the village of Parícutin, San Juan Parangaricutiro was buried beneath ash and lava .
Parícutin: The Volcano Born in a Mexican Cornfield, Edited by James F Luhr and Tom Simkin, Phoenix AZ: Geoscience Press, 1993. The definitive collection of reports and documentary illustrations of the eruption and its effects up to the date of publication. Peakbagger.com Parícutin: Credits. Retrieved April 16, 2008. Volcano World (El Jorullo).
Parícutin is a young volcano located 11 km northeast of Pico de Tancítaro. It first erupted in 1943 and remained active and grew in size until 1952. It first erupted in 1943 and remained active and grew in size until 1952.
Michoacán has a history of European immigrants including: Italians, Spaniards, and the French. There are small Italian communities found throughout the state including the cities of Nueva Italia, Michoacán and Lombardia in Michoacán, both founded by Dante Cusi from Gambar in Brescia. [77]
A monogenetic volcanic field is a type of volcanic field consisting of a group of small monogenetic volcanoes, each of which erupts only once, as opposed to polygenetic volcanoes, which erupt repeatedly over a period of time.
First volcano in the Cascades Volcanic Arc heading northwards, possibly the first volcanic eruption recorded using motion picture camera. Pyroclastic flows caused massive fires and evidence of the eruption still present in form of unusual growth patterns of trees as of 2020, 105 years later and charred trees.
Such cinder cones likely represent the final stages of activity of a mafic volcano. [11] However, most volcanic cones formed in Hawaiian-type eruptions are spatter cones rather than cinder cones, due to the fluid nature of the lava. [12] The most famous cinder cone, Paricutin, grew out of a corn field in Mexico in 1943 from a new vent. [3]