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occurred prior to this first day of the eruption. Once the cinder cone started erupting, it continued for 15 years, eventually stopping in 1774. El
Jorullo destroyed what had been a rich agricultural area. It grew approximately 820 feet (250 meters) from the ground in the first six weeks. The
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At the end of the first phase, after roughly one year, the cinder cone had grown 336 m (1,102 ft) tall. For the next eight years El Parícutin would continue erupting, although this was dominated by relatively quiet eruptions of lava that would scorch the surrounding 25 km
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Later eruptions from El
Jorullo were magmatic with neither mud nor water flows. This 15-year eruption was the longest one El Jorullo has had and was the longest cinder cone eruption known. Lava flows can still be seen to the north and west of the cinder cone. The eruption had a
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of ash and stones first-hand as they ploughed the field. El Parícutin grew quickly, reaching five stories tall in just a week, and it could be seen from afar in a month. Much of the volcano's growth occurred during its first year, while it was still in the explosive
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El
Jorullo has four smaller cinder cones which have grown from its flanks. The vents of El Jorullo are aligned in a northeast to southwest direction. Lava from these vents cover nine km around the volcano. Later eruptions produced lavas that had higher
464:, 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.
306:(9.7 sq mi) of land. The cinder cone's activity would slowly decline during this period until the last six months of the eruption, during which violent and explosive activity was frequent.
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In 1952 the eruption ended and Parícutin went quiet, attaining a final height of 424 m (1,391 ft) from the cornfield where it began. Like most
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Its current elevation is 1,320 meters (4,330 feet), and its crater is about 1,300 by 1,640 feet (400 by 500 meters) wide and 490 feet (150 meters) deep.
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The
Michoacán–Guanajuato volcanic field covers an area of 200 by 250 kilometres (120 mi × 160 mi), in the states of
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or on the flanks of eroded shield volcanoes. There are an average of 2.5 cinder cones every 100 kilometres (62 mi).
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farmer, Dionisio Pulido, on
February 20, 1943. Pulido, his wife, and their son all witnessed the initial
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phase. The nearby villages of
Paricutín (after which the volcano was named) and
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The cinder cones are randomly arranged and occur at low altitudes, usually, on
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were both buried in lava and ash. The residents relocated to nearby lands.
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Volcanic field in the
Michoacán and Guanajuato states of central Mexico
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The volcanic field is best known for the 18th-century eruption of
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415:. Smithsonian Institution, National Museum of Natural History
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cinder cone and the Cerro de Tancítaro shield volcano
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Video documentary (eng/spa) Volcano Parícutin (4min)
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in
Guanajuato. Other volcanoes in the field include
515:. Popular Science Monthly. Retrieved Apr. 17, 2008.
255:contents making them more viscous than the earlier
462:Parícutin: The Volcano Born in a Mexican Cornfield
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111:is located in the Michoacán and Guanajuato
484:. Volcano World. Retrieved Apr. 16, 2008.
322:lightning strikes caused by the eruptions
224:eruptions from El Jorullo were primarily
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521:. Bartleby.com. Retrieved Apr. 17, 2008.
435:"Michoacán-Guanajuato: Eruptive History"
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170:, a group of seven maars in and around
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142:volcano, and 20th-century eruption of
537:The eruption of Parícutin (1943-1952)
219:volcano began on September 29, 1759.
559:Michoacán–Guanajuato volcanic field
109:Michoacán–Guanajuato volcanic field
22:Michoacán–Guanajuato volcanic field
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377:San Juan Parangaricutiro Church
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135:(3860 m) is the highest peak.
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584:Natural history of Guanajuato
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52:3,860 m (12,660 ft)
589:Natural history of Michoacán
474:Volcano World (El Jorullo).
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478:. Retrieved April 17, 2008.
471:. Retrieved April 16, 2008.
166:in age. The field includes
115:of central Mexico. It is a
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457:Parícutin at Volcano World
365:Parícutin from Las Cabañas
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285:in a cornfield owned by a
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494:Global Volcanism Program
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413:Global Volcanism Program
300:San Juan Parangaricutiro
267:El Parícutin — 1943−1952
574:Volcanoes of Guanajuato
499:Smithsonian Institution
445:Smithsonian Institution
579:Volcanoes of Michoacán
489:"Michoacán-Guanajuato"
409:"Michoacán-Guanajuato"
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198:El Jorullo — 1759−1774
176:Alberca de los Espinos
519:"El Jorullo: Credits"
513:"El Jorullo: Credits"
482:"El Jorullo: Credits"
206:Drawing of El Jorullo
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123:field, with numerous
564:Volcanism of Mexico
389:Jorullo Cinder Cone
341:Cinder cone in 1943
315:monogenetic volcano
281:volcano began as a
476:Parícutin: Credits
469:Parícutin: Credits
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42:Highest point
261:basaltic andesite
178:in Michoacán and
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102:1943 to 1952
91:Cinder cones
296:pyroclastic
221:Earthquakes
164:Pleistocene
121:cinder cone
553:Categories
395:References
217:El Jorullo
212:El Jorullo
160:Guanajuato
150:Morphology
70:Guanajuato
504:April 16,
287:Purépecha
279:Parícutin
273:Parícutin
234:ash falls
193:Eruptions
156:Michoacán
146:volcano.
144:Parícutin
66:Michoacán
57:Geography
48:Elevation
34:Parícutin
291:eruption
226:phreatic
62:Location
419:23 July
328:Gallery
283:fissure
263:lavas.
257:basalts
140:Jorullo
80:Geology
253:silica
244:of 4.
113:states
74:Mexico
129:maars
506:2008
421:2022
277:The
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242:VEI
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