Parícutin in the context of "List of volcanoes in Mexico"

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⭐ Core Definition: Parícutin

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 presented the first occasion for modern science to document the full life cycle of an eruption of this type. During the volcano's nine years of activity, scientists sketched and mapped it and took thousands of samples and photographs. By 1952, the eruption had left a 424-meter-high (1,391 ft) cone and significantly damaged an area of more than 233 square kilometers (90 mi) with the ejection of stone, volcanic ash and lava. Three people were killed, two towns were completely evacuated and buried by lava, and three others were heavily affected. Hundreds of people had to permanently relocate, and two new towns were created to accommodate their migration. Although the larger region still remains highly active volcanically, Parícutin is now dormant and has become a tourist attraction, with people climbing the volcano and visiting the hardened lava-covered ruins of the San Juan Parangaricutiro Church.

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👉 Parícutin in the context of List of volcanoes in Mexico

Volcanoes in Mexico form a significant part of the country's geological landscape, with numerous active and extinct volcanoes primarily located along the central-southern Trans-Mexican Volcanic Belt. The diverse array of volcanic features in Mexico includes stratovolcanoes, shield volcanoes, cinder cones, lava domes, and calderas.

Many of Mexico's volcanoes are part of the Pacific Ring of Fire, a region characterized by frequent earthquakes and volcanic eruptions. Notable volcanoes 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.Volcanoes play a significant role in Mexico's geography, climate, and culture, influencing local ecosystems, agriculture, and human settlements. The volcanic activity also poses hazards to surrounding communities, necessitating ongoing monitoring and disaster preparedness efforts.

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Parícutin in the context of Basaltic andesite

Basaltic andesite or andesibasalt is a volcanic rock that is intermediate in composition between basalt and andesite. It is composed predominantly of augite and plagioclase. Basaltic andesite can be found in volcanoes around the world, including in Central America and the Andes of South America.

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Parícutin in the context of Monogenetic volcanic field

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. The small monogenetic volcanoes of these fields are the most common subaerial volcanic landform.

Many monogenetic volcanoes are cinder cones, often with lava flows, such as Parícutin in the Michoacán-Guanajuato volcanic field, which erupted from 1943 to 1952. Some monogenetic volcanoes are small lava shields, such as Rangitoto Island in the Auckland volcanic field. Other monogenetic volcanoes are tuff rings or maars. A monogenetic field typically contains between ten and a hundred volcanoes. The Michoacán-Guanajuato field in Mexico contains more than a thousand volcanoes and is exceptionally large.

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LINKED FROM (PARENTS)
← Basaltic andesite ← List of volcanoes in Mexico ← Monogenetic volcanic field
LINKS TO (CHILDREN)
Cinder cone → Volcano → Michoacán → Uruapan → Mexico City → Volcanic ash → Lava →