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List Of Volcanoes In Mexico
Types of volcanoes There are multiple types of volcanoes in Mexico. Volcanoes can be of different types such as cinder cone volcanoes, composite volcanoes, shield volcanoes, and lava domes. Each of these variations of volcanos forms in its own way. Cinder cone volcanoes are the simplest type of volcano. This volcano forms from particles of solidified lava that ejected from a single vent. When the lava is eruptive and blows into the air, it separates into small fragments that solidify and fall around the central vent to form an oval cone at the top of the volcano. “Composite volcanoes or stratovolcanoes, make up some of the world’s most memorable mountains: Mount Rainier, Mount Fuji, and Mount Cotopaxi.” These volcanoes are very steep sided and symmetrical, in a cone shape. They have a conduit system which allows the magma to flow from deep within the Earth’s surface. They have many vents within the volcano which allows the lava to break through the walls, which allows ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Map Mexico Volcanoes
A map is a symbolic depiction emphasizing relationships between elements of some space, such as objects, regions, or themes. Many maps are static, fixed to paper or some other durable medium, while others are dynamic or interactive. Although most commonly used to depict geography, maps may represent any space, real or fictional, without regard to context or scale, such as in brain mapping, DNA mapping, or computer network topology mapping. The space being mapped may be two dimensional, such as the surface of the earth, three dimensional, such as the interior of the earth, or even more abstract spaces of any dimension, such as arise in modeling phenomena having many independent variables. Although the earliest maps known are of the heavens, geographic maps of territory have a very long tradition and exist from ancient times. The word "map" comes from the , wherein ''mappa'' meant 'napkin' or 'cloth' and ''mundi'' 'the world'. Thus, "map" became a shortened term referring to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Durango Volcanic Field
Durango volcanic field is a volcanic field in north-central Mexico (Durango), east of the Sierra Madre Occidental. The field covers a surface area of . The volcanic field is located in the Tepehuano terrane. Volcanism in the area was accompanied by tectonic extension. There are around hundred cones in the field. Some volcanic rocks have been affected by faulting; buried faults are also found. The San Luis-Tepehuanes fault system is associated with the field. The whole field is covered by lavas, which are about thick and reach a total volume of . Magma ascent has been controlled by northwest-trending faults. Volcanism in the wider territory was related to the subduction of the Farallon plate until 29 mya. Later tectonic changes caused a start of more alkaline volcanism. The volcanoes have erupted basanite. The main components of the rocks at La Breña-El Jagüey are clinopyroxene, ilmenite, olivine, plagioclase and titanomagnetite, with rocks sporting variable textures. The par ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nevado De Toluca
Nevado de Toluca () is a stratovolcano in central Mexico, located about 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. Etymology It is often called by the Nahuatl name Xinantecatl which is usually translated as The Naked Lord, ''Señor Desnudo'' in Spanish, although other etymologies have been suggested such as "Lord of the Corn Stalks", Tzinacantecatl or Zinacantepetl (Mountain of the Bats). Further evidence regarding the etymologies of this mountain has surfaced after many archeology discoveries in and around the area. It has been concluded that its correct etymology is Chicnauhtecatl meaning "Lord of Nine", probably referring to the various deep lakes at the top of the cone. Description The volcano has a wide summit caldera which is open to the east. The highest summit, the Pico del Fraile (Friar's Peak), is on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Naolinco Volcanic Field
Naolinco volcanic field is a volcanic field in Veracruz, Mexico. It lies in the region of the cities of Jalapa and Naolinco, and the town of Naolinco lies in the field. Geologic context The Trans-Mexican Volcanic Belt is best known for calc-alkaline volcanoes such as Pico de Orizaba and Popocatepetl stratovolcanoes as well as calderas and pyroclastic cones; however it also features scattered alkali basalt volcanism. It lies at an angle to the Middle America Trench unlike the more typical volcanic arcs of Central America; some theories consider the belt to be independent from the trench. In its eastern region lies the Cofre de Perote and a group of volcanoes including the Naolinco Volcanic Field. Sometimes it and some neighbouring monogenetic volcanoes such as those at Cofre de Perote are included into a "Xalapa volcanic field", which would have about 50 volcanic centres. Despite their location, they are most likely unrelated to Cofre de Perote itself. The field The N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moctezuma Volcanic Field
Moctezuma volcanic field is a volcanic field in Sonora, Mexico. The towns of Moctezuma, La Junta, Casa Grande, San Clemente de Terapa, Tepache, El Llano and Divisaderos lie in the area. Volcanic activity in Mexico encompasses both oceanic and continental types of volcanic activity. Geographically, volcanism in Mexico is often subdivided into a Californian, Eastern Alcalic, Sierra Madre Occidental and Trans-Mexican Volcanic Belt, with the addition of a fifth proposed in 2007, which is known as the Northern Mexico Extensional Province. The field is located in the Moctezuma basin, in central Sonora on the western foot of the Sierra Madre Occidental range. The ranges immediately east and west of the Moctezuma basin are known as Sierra La Madera and Sierra El Coyote, respectively. This is a sedimentary basin delimited by faults; the basin is part of the Basin and Range Province of the state of Sonora. The oldest rocks are of Cretaceous age and a number of fossils have been investig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Michoacán–Guanajuato Volcanic Field
Michoacán–Guanajuato volcanic field is located in the Michoacán and Guanajuato states of central Mexico. It is a volcanic field that takes the form of a large cinder cone field, with numerous shield volcanoes and maars. Pico de Tancítaro (3860 m) is the highest peak. The volcanic field is best known for the 18th-century eruption of Jorullo volcano, and 20th-century eruption of Parícutin volcano. Morphology The Michoacán–Guanajuato volcanic field covers an area of , in the states of Michoacán and Guanajuato. It contains 1400 vents, mostly cinder cones. The shield volcanoes are mostly Pleistocene in age. The field includes Siete Luminarias, a group of seven maars in and around Valle de Santiago in Guanajuato. Other volcanoes in the field include Alberca de los Espinos in Michoacán and Cerro Culiacán in Guanajuato. The cinder cones are randomly arranged and occur at low altitudes, usually, on alluvial plains or on the flanks of eroded shield volcanoes. There ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Malinche (volcano)
La Malinche, also known as Matlalcueye or Malintzin, is an active volcano (dormant for the last 3,100 years) located in the states of Tlaxcala and Puebla in Mexico. Officially, its summit reaches above sea level, though it is generally considered to be closer to , using GPS measurements. It is the highest peak in Tlaxcala, the fifth-highest in Puebla, the sixth-highest in Mexico, the 23rd-highest in North America, and the 252nd-highest in the world. Its height above nearby cities varies from above Huamantla, above Villa Vicente Guerrero, above Tlaxcala, to above Puebla. The summit is from Tlaxcala, from Puebla, and from Mexico City. The climate is cold near the summit and mild on the lower slopes. The Tlaxcaltecs named the peak ''Matlalcueitl'', which translates to " ady of theBlue Skirt", a goddess of rain and song, believed to be the local equivalent of Chalchiuhtlicue. The Spanish named it simply ''Sierra de Tlaxcala'' ("Tlaxcalan Range"). The current name, ''Mal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
El Jorullo
El Jorullo is a cinder cone volcano in Michoacán, central Mexico, on the southwest slope of the central plateau, 33 miles (53 kilometers) southeast of Uruapan in an area known as the Michoacán-Guanajuato volcanic field. It is about 6 miles (10 km) east-northeast of La Huacana. Its current elevation is . 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 square km around the volcano. Later eruptions produced lavas that had higher silica contents making them thicker than the earlier basalts and basaltic andesite lavas. El Jorullo's crater is about 1,300 by 1,640 feet (400 by 500 m) wide and 490 feet (150 m) deep. El Jorullo is one of two known volcanoes to have developed in Mexico in recent history. The second, born about 183 years later, was named Parícutin after a nearby village that it eventually destroyed. P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jocotitlán (volcano)
Jocotitlán, also known as Xocotépetl (), is a volcano in the Jocotitlán and Atlacomulco municipalities, in the State of Mexico. At above sea level, its summit is the 12th highest peak of Mexico. Jocotitlán volcano lies in the northern part of the Toluca Valley. It is part of the Eje Neovolcánico, a volcanic belt that traverses south-central Mexico. It is a stratovolcano formed by tephra and solidified lava flows. The volcano lies within the Isidro Fabela state park, a protected area of 3701 ha established in 1975. Jocotitlán was considered holy by the Mazahua and Otomi peoples. The former called it ''Nguemore'' ("sacred mountain"), while the latter called it ''Gumidi'' ("he who sits facing straight forward"). In Pre-Columbian Mexico, the volcano held a sanctuary for Otontecuhtli, the Otomi king of the gods, also known to the Nahua people as fire god Xiuhtecuhtli. The volcano has also held a Catholic chapel since the 1980s. At , it is probably one of the highest ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jaraguay Volcanic Field
Jaraguay volcanic field is a volcanic field in northern Baja California, Mexico. Jaraguay volcanic field is part of a chain of volcanic fields that formed on the Baja California peninsula after subduction of the Pacific plate beneath it ceased. Starting from the north they are San Quintín, Jaraguay, San Borja, Santa Clara, San Ignacio–San José de Gracia, Santa Rosalía and La Purísima (volcano) volcanic fields. The field consists of cinder cones and lava flows. The lavas cover a surface area of and tend to have thicknesses . Many of these were erupted from fissures with no clear vents. Cinder cones have average heights of above basis. There is some geographical differentiation with the largest cones found on the western side and the cones concentrated on the easternmost edge. A flat lava plateau also makes up the field. Approximately 214 vents were counted in 2013. Many of these vents are elongated in north-south direction, with a slight NNW-SSE slant. Rocks erupted in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iztaccihuatl
Iztaccíhuatl (alternative spellings include Ixtaccíhuatl, or either variant spelled without the accent) ( or, as spelled with the x, ), is a dormant volcanic mountain in Mexico located on the border between the State of Mexico and Puebla within Izta-Popo Zoquiapan National Park. It is the nation's third highest, after Pico de Orizaba at , and Popocatépetl at . The name "Iztaccíhuatl" is Nahuatl for "White woman", reflecting the four individual snow-capped peaks which depict the head, chest, knees and feet of a sleeping female when seen from east or west. Iztaccíhuatl is to the north of its twin Popocatépetl, to which it is connected by the high altitude Paso de Cortés. Depending on atmospheric conditions Iztaccíhuatl is visible much of the year from Mexico City some to the northwest. The first recorded ascent was made in 1889, though archaeological evidence suggests the Aztecs and previous cultures climbed it previously. It is the lowest peak containing permanent sno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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