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Paricutin stands near the city of Uruapan in southwestern Mexico, about two hundred miles west of Mexico City. It received its name from the village of Paricutin. This volcano is rare because scientists were able to watch the birth, growth, and the death of it. Geologists from many parts of the world came to study this vast volcanic event and from then on it was un
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Three weeks before the eruption, the people near Paricutin village heard the rumbling noises that resembled thunder, but they were confused because the skies were clear and there were no clouds. The eruption that created Paricutin began in a cornfield on February 20, 1943 and continued through 1952 from a crack in the earth. A farmer, Dionisio Pulido, and his wife witnessed this happen. The rate of eruption steadily lowered until the last six months of the eruption when violent explosions were frequent and violent.
No one was killed by the lava or ash, but three people were killed by lightning associated with the eruption. The final height of the scoria cone was four hundred and twenty-four meters. Also along with scientists, many people from all around the world came to observe it. The volcano showed vulcanian-type activity, with large canon-like explosions separated by short periods of silence. They said they saw “the earth crack before-them and smoke rise that smelled like a rotten egg. Lava flows covered about ten square miles and had a volume of about 0. ” Most of the explosive activity was during the first year of the eruption when the cone grew to 1,100 feet and lava rose to about fifty feet above the crater's rim.
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