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Popocatépetl (UK: / ˌ p ɒ p ə ˈ k æ t ə p ɛ t əl, ˌ p ɒ p ə k æ t ə ˈ p ɛ t əl / POP-ə-KAT-ə-pet-əl, -kat-ə-PET-əl, US: / ˌ p oʊ p-/ POHP-, Spanish: [popokaˈtepetl] ⓘ; Nahuatl languages: Popōcatepētl [popoːkaˈtepeːt͡ɬ] ⓘ) is an active stratovolcano located in the states of Puebla, Morelos, and Mexico in central Mexico.
The final eruptions in the creation of Banks Peninsula in New Zealand occurred about 9 million years ago. A major eruption of Gran Canaria took place around 14 million years ago. Approximately 23.03 million years BP, the Neogene period and Miocene epoch begin. Cerro Guacha, Bolivia; 5.6–5.8 Ma (Guacha ignimbrite). [61]
View of the Puebla Valley, with Popocatépetl and Iztaccíhuatl in the distance, 1906. Popocatépetl and Iztaccíhuatl refers to the volcanoes Popocatépetl ("the Smoking Mountain") and Iztaccíhuatl ("sleeping woman" in Nahuatl, sometimes called the Mujer Dormida "sleeping woman" in Spanish) [1] in Iztaccíhuatl–Popocatépetl National Park, [2] [3] which overlook the Valley of Mexico and ...
The volcano was inactive for decades before an eruption in 1994. In 2000, a major eruption prompted the evacuation of about 50,000 people in the region. Since then, mild to moderate activity has ...
Mexico’s National Disaster Prevention Center said Wednesday the Popocatépetl volcano, located just 50 miles from the country's capital, has erupted 13 times in the past day and urged people to ...
1883 eruption of Krakatoa: 30,000 Mount Pelée: 4 Martinique: 1902 1902 eruption of Mount Pelée: 23,000 Nevado del Ruiz: 3 Colombia: 1985 Armero tragedy: 20,000~ (estimated) Santorini: 6 Greece: c. 1600 BC Minoan eruption: 15,000 to 20,000 Mount Samalas: 7 Indonesia: 1257 1257 Samalas eruption: 15,000 Mount Unzen: 2 Japan: 1792 1792 Unzen ...
While east of the mountain residents swept streets and didn’t remove their masks on Tuesday, here to the west, they casually watched the gas and ash plume emerging from its crater. The 17,797 ...
The first event took place from 1857 to 1868 which caused by the historic eruption of Tacaná, two years prior. A year later after the eruption of the Santa Maria volcano, the second suppression event started from 1903 to 1908, during which tree growth was affected by the thickness of ash fall from the eruption and deposited near each tree. [10]