Michoacán-Guanajuato Volcano
Michoacán-Guanajuato volcanic field is mostly known for Paricutín, one of the few volcanoes whose birth has been witnessed by man. It literally grew over a corn-field during 1943-52!
The widespread Michoacán-Guanajuato volcanic field contains over 1400 vents, including the historically active cinder cones of Parícutin and Jorullo, covering a 200 x 250 km wide area of Michoacán and Guanajuato states in west-central México. Cinder cones are the predominant volcanic form, but small shield volcanoes, lava domes, maars and tuff rings (many in the Valle de Santiago area), and coneless lava flows are also present.
Michoacán-Guanajuato volcano eruptions: 1759-74 (Jorullo), 1943-52 (Paricutín)
radiocarbon- or archeology dated:
1050 ± 50 years (?, Valle de Santiago), 1880 BC ± 150 years (Cerro el Jabali), ca. 2050 BC (Valle de Santiago, La Alberca), 2750 BC ± 200 years (Cerro el Metate), 6480 BC ± 300 years (Cerro la Taza), 7350 BC ± 300 years (Hoyo el Huanillo)
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Background
The shield volcanoes of the Michoacán-Guanajuato volcanic field are mostly Pleistocene in age, and have morphologies similar to small Icelandic-type shield volcanoes, although the Michoacán-Guanajuato shields have higher slope angles and smaller basal diameters. Jorullo, which was constructed in the 18th century, and Parícutin are the two best known of the roughly 1000 small volcanic centers scattered throughout the volcanic field.Significant volcanic eruptions: Michoacán-Guanajuato volcano
There is one uncertain or discredited eruption around 1050 AD from Michoacán-Guanajuato volcano.
| Date | Note | VEI | Deaths | Damage | |
|---|---|---|---|---|---|
| Parícutin Historical obs./docs. | 4 | ||||
| 1943 Feb 20 (eruption | Historical obs./docs. | 4 | 103 | Info | |
| Jorullo Historical obs./docs. | 4 | ||||
?? | Uncertain Eruption | ? | |||
| Cerro el Zoyate | ? | ||||
| Cerro el Jabalí | 3 | ||||
| Valle de Santiago (La Alberca) | ? | ||||
| Cerro el Metate | 3 | ||||
| Cerro la Tinaja | ? | ||||
| Cerro Grande? | ? | ||||
| Cerro la Taza | 3 | ||||
| Hoyo el Huanillo | 3 | ||||
Eruptions of Michoacán-Guanajuato volcano
Paricutin was formed as a new volcano on 20 February 1943 in Mexico. A fissure opened on a corn field on the lands of Rancho Tepacua. A new fissure opened and started to erupt lava, forming a new cinder cone and a vast lava flow that destroyed Paricutin village, but spared its church. ...more info
A violent eruption started in June 1959 from a new fissure and lasted until 1774, building the 350 m tall Jorullo cone and several smaller new cones. ...more info
Michoacán-Guanajuato Volcano FAQ
+When was the last eruption of Michoacán-Guanajuato volcano?
The last confirmed eruption of Michoacán-Guanajuato occurred during 1943 - 1952.
+How often does Michoacán-Guanajuato volcano erupt?
Since 1759, Michoacán-Guanajuato volcano has had at least 2 historically documented eruptions. This means that it erupts on average every 133 years.
Many eruptions of Michoacán-Guanajuato have lasted more than one year. In total, the volcano has been in eruption during 26 out of 266 years until now. In other words, Michoacán-Guanajuato has been active at least one in 10.2 years on average. Note that this value is likely an underestimate, because the known history of eruptions from Michoacán-Guanajuato is likely incomplete, especially further back in time.
+How active is Michoacán-Guanajuato volcano at present?
Michoacán-Guanajuato volcano is infrequently active: Since 1900, it has had 10 eruptions, and been active during 10 years out of 126 as of now. This means, Michoacán-Guanajuato has been in eruption one in 12.6 years on average. The last eruption was from 1943 until 1952 and ended 74 years ago.
+When was the largest eruption of Michoacán-Guanajuato volcano?
The largest eruption of Michoacán-Guanajuato volcano in historic times occurred during 1943 - 1952. It ranks as a sub-plinian eruption with a magnitude 4 on the VEI (Volcanic Explosivity Index) scale.
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Michoacán-Guanajuato Volcano Maps




































