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Geological Formation

Paricutin

Volcanic Formations

Paricutin is a cinder cone volcano in Michoacan state, Mexico, about 29 kilometers west of Uruapan, part of the Michoacan-Guanajuato volcanic field within the Trans-Mexican Volcanic Belt, built from basaltic andesite lava and reaching 2,800 meters above sea level, with its cone rising 424 meters above the surrounding valley floor. It is famous for having been born on February 20, 1943, when it burst suddenly out of a cornfield belonging to farmer Dionisio Pulido, building a scoria cone 50 meters high within its first 24 hours through strombolian pyroclastic activity. The eruption continued for nine years, an unusually long lifespan for a cinder cone, unfolding across four distinct phases before ending in 1952. Because scientists were able to observe and document its entire life cycle from birth to dormancy, Paricutin became the first volcano of its kind ever fully documented in this way, and it remains geothermally active today with residual steam emissions and seismicity. This entity documents Paricutin specifically as a geological formation, a cinder cone volcano whose complete nine-year life cycle from birth in a cornfield was the first ever fully documented.

Facts
Activity
Dormant 1
Visitor Access
Open 1
Classification
Protected Status
IUGS Geological Heritage Site 1
Connections

Caused By

Volcanism, Processes

Wikidata P31 formation-type mapped to formative process Volcanism via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Parícutin (Wikipedia)

In Discipline

Wikidata P31 formation-type mapped to discipline Volcanology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.

Source Wikidata: Paricutin
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Found In

Also in Geography Atlas: where this subject is found.

Source Wikidata: Paricutin
Sources
1. Parícutin (Wikipedia)
  • Lead paragraph
    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.
  • Category: Second 100 IUGS Geological Heritage Sites
    Wikipedia category: Second 100 IUGS Geological Heritage Sites
  • Caused By: Volcanism, Lead, process Volcanism
    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 mi2) with the ejection of stone, volcanic ash and lava.
View the Source
Wikidata: Paricutin
Wikidata Q231620, class allow-list match (w-wdresolver-0926)View the Source
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