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Matlalcueitl (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] |
Cordillera Anahuac
A cordillera is an extensive chain and/or network system of mountain ranges, such as those in the west coast of the Americas. The term is borrowed from Spanish, where the word comes from , a diminutive of ('rope'). The term is most commonly used in physical geography p. 687 (Encyclopedia Americana Corp., 1918): "It is used particularly in physical geography, although in geology also it is sometimes applied...." and is particularly applied to the various large |
Tlaxcaltec
The Tlaxcalans, or Tlaxcaltecs, are a Nahua people who live in the Mexican state of Tlaxcala. Pre-Columbian history The Tlaxcaltecs were originally a conglomeration of three distinct ethnic groups who spoke Nahuatl, Otomi, and Pinome that comprised the four city-states of the Tlaxcala Confederation. Eventually, the Nahuatl speakers became the dominant ethnic group. Despite early attempts by the Mexica, the Tlaxcaltecs were never conquered by the Aztec Triple Alliance. Some of the wars between the Tlaxcalans and the Aztecs are called the xochiyaoyatl (flower wars), as their objective was not to conquer but rather to capture enemy warriors for sacrifice.Hassig, Ross (1988). ''Aztec Warfare: Imperial Expansion and Political Control''. Norman: University of Oklahoma Press. p. 130. . Spanish colonial history Eager to overthrow the Aztecs, which were their hated enemies, the Tlaxcaltecs allied with Hernán Cortés and his fellow Spanish conquistadors and were instrumental in the inv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pinus Montezumae
''Pinus montezumae'', known as the Montezuma pine, is a species of conifer in the family Pinaceae. It is native to Mexico and Central America, where it is known as ocote. The tree grows about 35 m high and 80 cm in diameter; occasionally it may reach a height of 40 m and diameter of 1 m. It has a round crown. The bark is dark brown-grayish. It is the only pine species (in the variety ''rudis'') which has seven needles in each fascicle. It is found from the Mexican states of Nuevo León (25° N. Lat.) and Jalisco (22° n.l.) to the north and to Nicaragua (15° N. Lat.) to the south. It occurs on both mountain ranges of the Sierra Madre Oriental and Sierra Madre Occidental. It grows at altitudes from 2000–3200 m above sea level. It is found in areas between 800–1000 mm rainfall per year. In most of the tree's habitat, rain falls mostly in summer, but in the state of Veracruz, precipitations are spread year round and the climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alnus Acuminata
''Alnus acuminata'' is a species of deciduous tree in the Betulaceae family. It is found in montane forests from central Mexico to Argentina.Zuloaga, F. O., O. N. Morrone, M. J. Belgrano, C. Marticorena & E. Marchesi. (eds.) 2008. Catálogo de las plantas vasculares del Cono Sur. Monographs in systematic botany from the Missouri Botanical Garden 107(1–3): i–xcvi, 1–3348. Description ''Alnus acuminata'' grows up to tall with a straight trunk up to thick. The bark has many yellowish lenticels. The leaves are simple, oval with toothed margins. The inflorescences are catkins, separate male and female flowers on the same tree. The male flowers are up to long and pendulous, while the smaller female flowers are green, erect and resemble a small cone A cone is a three-dimensional geometric shape that tapers smoothly from a flat base (frequently, though not necessarily, circular) to a point called the apex or vertex. A cone is formed by a set of line segments, half-lin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cerro Xalapasco Vista
Cerro is Spanish for "hill" or "mountain". Toponyms ;Bolivia: * Cerro Rico, the "Rich Mountain" containing silver ore near Potosi, Bolivia ;Brazil: *Cerro Branco, a municipality of Rio Grande do Sul *Cerro Grande, Rio Grande do Sul, a municipality of Rio Grande do Sul * Cerro Largo, a municipality of Rio Grande do Sul ;Chile * Cerro de Los Inocentes, in the Juan Fernández Islands ;Cuba: * Cerro, Havana, a district (''municipio'') ;Italy: *Cerro (Bottanuco), a subdivision of Bottanuco in the province of Bergamo *Cerro al Lambro, in the province of Milano *Cerro al Volturno, in the province of Isernia *Cerro Maggiore, in the province of Milano *Cerro Tanaro, in the province of Asti *Cerro Veronese, in the province of Verona ;Mexico: * Cerro Potosí ;United States: * Cerro, New Mexico ;Uruguay: * Cerro Largo Department * Villa del Cerro, in Montevideo * Fortaleza del Cerro, in Montevideo Football clubs * C.A. Cerro, a football club from Montevideo, Uruguay * Club Cerro Cor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyramidal Peak
A pyramidal peak, sometimes called a glacial horn in extreme cases, is an angular, sharply pointed mountain peak which results from the cirque erosion due to multiple glaciers diverging from a central point. Pyramidal peaks are often examples of nunataks. Formation Glaciers, typically forming in drainages on the sides of a mountain, develop bowl-shaped basins called cirques (sometimes called ‘corries’ - from Scottish Gaelic ʰəɾə(a bowl) - or s). Cirque glaciers have rotational sliding that abrades the floor of the basin more than walls and that causes the bowl shape to form. As cirques are formed by glaciation in an alpine environment, the headwall and ridges between parallel glaciers called arêtes become more steep and defined. This occurs due to freeze/thaw and mass wasting beneath the ice surface. It is widely held that a common cause for headwall steepening and extension headward is the crevasses known as bergschrund that occur between the moving ice and the he ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Cone
Volcanic cones are among the simplest volcanic landforms. They are built by ejecta from a volcanic vent, piling up around the vent in the shape of a cone with a central crater. Volcanic cones are of different types, depending upon the nature and size of the fragments ejected during the eruption. Types of volcanic cones include stratocones, spatter cones, tuff cones, and cinder cones. Stratocone Stratocones are large cone-shaped volcanoes made up of lava flows, explosively erupted pyroclastic rocks, and igneous intrusives that are typically centered around a cylindrical vent. Unlike shield volcanoes, they are characterized by a steep profile and periodic, often alternating, explosive eruptions and effusive eruptions. Some have collapsed craters called calderas. The central core of a stratocone is commonly dominated by a central core of intrusive rocks that range from around to over several kilometers in diameter. This central core is surrounded by multiple generations of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (annum, Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphy, stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, evolution of mammals, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Picos De La Malinche
Picos is a municipality in the state of Piauí in the Northeast region of Brazil. Picos is the state's third-largest city, located in the south-central region of Piauí and is the most economically developed city in the region. The city's financial prosperity, combined with its geographical location, gives Picos a "commercial hub" status, especially for fuel and honey (Picos is known as the "capital of honey"). As of 2020, the population was approximately 78,431. Climate According to data from INMET - National Institute of Meteorology, the city of Picos Piauí has average annual temperature of . Demographics The population of the city of Picos is currently 78,431 inhabitants (IBGE 2020), and 58,307 in urban areas and 15,107 in rural areas, thus characterizing the third largest city from Piaui. It has a population density of 137.23 inhabitants / km ². Neighborhoods and Villages Villages Villages include Coroatá, Fátima do Piauí, Gameleira dos Rodrigues, Lagoa Grande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Parque Nacional La Malinche
La Malinche National Park is located in the states of Puebla and Tlaxcala in Central Mexico. The park is east of Mexico City, and about from the capital city of Tlaxcala, Tlaxcala. Volcano The La Malinche—Matlalcueitl volcano, part of the Trans-Mexican Volcanic Belt, is within the park. The volcano has an elevation of above sea level. It is frequently used by mountaineers for training and altitude acclimatization before climbing the higher volcanos in the region. The volcano's slope is gentle, and its vicinity to Mexico City makes it a popular weekend destination. A paved road reaches the top of the volcano. The "Centro Vacacional IMSS La Malintzi" on the volcano has 40 cabins, a camping area and some recreational facilities. See also *List of national parks of Mexico *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 volcanoe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conquest Of The Aztec Empire
The Spanish conquest of the Aztec Empire, also known as the Conquest of Mexico or the Spanish-Aztec War (1519–21), was one of the primary events in the Spanish colonization of the Americas. There are multiple 16th-century narratives of the events by Spanish conquistadors, their indigenous allies, and the defeated Aztecs. It was not solely a contest between a small contingent of Spaniards defeating the Aztec Empire but rather the creation of a coalition of Spanish invaders with tributaries to the Aztecs, and most especially the Aztecs' indigenous enemies and rivals. They combined forces to defeat the Mexica of Tenochtitlan over a two-year period. For the Spanish, the expedition to Mexico was part of a project of Spanish colonization of the New World after twenty-five years of permanent Spanish settlement and further exploration in the Caribbean. Significant events in the conquest of Mesoamerica Historical sources for the conquest of Mexico recount some of the same events ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hernán Cortés
Hernán Cortés de Monroy y Pizarro Altamirano, 1st Marquess of the Valley of Oaxaca (; ; 1485 – December 2, 1547) was a Spanish ''conquistador'' who led an expedition that caused the fall of the Aztec Empire and brought large portions of what is now mainland Mexico under the rule of the King of Castile in the early 16th century. Cortés was part of the generation of Spanish explorers and conquistadors who began the first phase of the Spanish colonization of the Americas. Born in Medellín, Spain, to a family of lesser nobility, Cortés chose to pursue adventure and riches in the New World. He went to Hispaniola and later to Cuba, where he received an '' encomienda'' (the right to the labor of certain subjects). For a short time, he served as '' alcalde'' (magistrate) of the second Spanish town founded on the island. In 1519, he was elected captain of the third expedition to the mainland, which he partly funded. His enmity with the Governor of Cuba, Diego Velázquez de Cu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
