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Iztaccíhuatl or Ixtaccíhuatl (both forms also spelled without the accent) (Nahuatl pronunciation: [istakˈsiwat͡ɬ] ⓘ or, as spelled with the x, [iʃtakˈsiwat͡ɬ]) is a 5,230 m (17,160 ft) [1] dormant volcanic mountain in Mexico located on the border between the State of Mexico and Puebla within Izta-Popo Zoquiapan National Park.
In 1978, geophysicists Glen Penfield and Antonio Camargo were working for the Mexican state-owned oil company Petróleos Mexicanos as part of an airborne magnetic survey of the Gulf of Mexico north of the Yucatán Peninsula. [14]: 20–21 Penfield's job was to use geophysical data to scout possible locations for oil drilling. [5]
Volcanoes in Mexico form a significant part of the country's geological landscape, with numerous active and extinct volcanoes scattered throughout the nation. These volcanoes are primarily located within the Trans-Mexican Volcanic Belt , a major volcanic arc in North America that extends across central-southern Mexico.
At 5,393 m (17,694 ft) [1] it is the second highest peak in Mexico, after Citlaltépetl (Pico de Orizaba) at 5,636 m (18,491 ft). It is linked to the twin volcano of Iztaccihuatl to the north by the high saddle known as the "Paso de Cortés". [5] Izta-Popo Zoquiapan National Park, wherein the two volcanoes are located, is named after them. [6] [7]
Name Elevation Location Last eruption meters feet Coordinates; Malumalu: Last 8,000 years Ta‘u-931: 3054: 30,000 years ago [15]: Ofu-Olosega: 639: 2096: 1866 unnamed submarine cone eruption
On Sunday, officials raised the volcano threat level to "Yellow Phase 3," which calls for those who live nearest to the volcano — including the 2,000 residents of Santiago Xalitzintla — to ...
Nevado de Toluca (Spanish: [neˈβaðo ðe toˈluka] ⓘ) is a stratovolcano in central Mexico, located about 80 kilometres (50 mi) west of Mexico City near the city of Toluca. It is the fourth highest of Mexico's peaks, after Pico de Orizaba, Popocatépetl and Iztaccíhuatl. The volcano and the area around it is now a national park.
The Central American Volcanic Arc (often abbreviated to CAVA) is a chain of volcanoes which extends parallel to the Pacific coastline of the Central American Isthmus, from Mexico to Panama. This volcanic arc, which has a length of 1,100 kilometers (680 mi) [ 1 ] [ 2 ] is formed by an active subduction zone, with the Cocos plate subducting ...