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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.
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).
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 .
Notable volcanoes in Mexico include Popocatépetl, one of the country's most active and dangerous volcanoes, Pico de Orizaba (Citlaltépetl), the highest peak in Mexico, and Parícutin, a cinder cone volcano that famously emerged from a cornfield in 1943. Mexican volcanoes play a significant role in the country's geography, climate, and culture ...
Parícutin, the Mexican cinder cone which was born in a cornfield on February 20, 1943, and Sunset Crater in Northern Arizona in the US Southwest are classic examples of cinder cones, as are ancient volcanic cones found in New Mexico's Petroglyph National Monument.
A volcano on an uninhabited island in the Galapagos has begun erupting, lighting up the nighttime sky as lava tumbled down its sides toward the sea. The La Cumbre volcano on Fernandina island ...
An undersea volcano erupted off Japan three weeks ago, providing a rare view of the birth of a tiny new island, but experts say it may not last very long. The unnamed undersea volcano, located ...
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]