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Cerro Tláloc
Cerro Tláloc (sometimes wrongly listed as ''Cerro el Mirador''; Nahuatl: ''Tlalocatépetl'') is a mountain and archaeological site in central Mexico. It is located in the State of Mexico, in the municipalities of Ixtapaluca and Texcoco, State of Mexico, Texcoco, close to the state border with Puebla. Formerly an active volcano, it has an elevation of , thus being the ninth highest mountain of Mexico. The mountain was considered by the Nahua people, Nahuan peoples, foremost among them the Aztecs, to be specially sacred to the raingod Tláloc. In fact, the mountain was believed to be one of his primary earthly dwelling places, called Tlālōcān. Attribution of this and other mountains to the sacred presence of rain deities predates the Aztec era by centuries, even millennia. At the summit there are still remains of a shrine where high ceremonies would have been carried out. The rites of Tláloc were otherwise performed at his temples, most famously that occupying one half of the T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nahua People
The Nahuas ( ) are a Uto-Aztecan languages, Uto-Nahuan ethnicity and one of the Indigenous people of Mexico, with Nahua minorities also in El Salvador, Guatemala, Honduras, Nicaragua, and Costa Rica. They comprise the largest Indigenous group in Mexico, as well as the largest population out of any North American Indigenous people group who are native speakers of their respective Indigenous languages of the Americas, Indigenous language. Amongst the Nahua, this is Nahuatl. When ranked amongst all Indigenous languages across the Americas, Nahuas list third after speakers of Guarani language, Guaraní and Quechuan languages, Quechua. The Mexica (Aztecs) are of Nahua ethnic group, ethnicity, as are their historical enemies and allies of the Spaniards: the Tlaxcaltec, Tlaxcallans (Tlaxcaltecs). The Toltecs which predated both groups are often thought to have been Nahua as well. However, in the pre-Columbian period Nahuas were subdivided into many groups that did not necessarily share ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Late Pleistocene
The Late Pleistocene is an unofficial Age (geology), age in the international geologic timescale in chronostratigraphy, also known as the Upper Pleistocene from a Stratigraphy, stratigraphic perspective. It is intended to be the fourth division of the Pleistocene Epoch within the ongoing Quaternary Period. It is currently defined as the time between 129,000 and c. 11,700 years ago. The late Pleistocene equates to the proposed Tarantian Age of the geologic time scale, preceded by the officially ratified Chibanian (commonly known as the Middle Pleistocene). The beginning of the Late Pleistocene is the transition between the end of the Penultimate Glacial Period and the beginning of the Last Interglacial around 130,000 years ago (corresponding with the beginning of Marine Isotope Stage 5). The Late Pleistocene ends with the termination of the Younger Dryas, some 10th millennium BC, 11,700 years ago when the Holocene Epoch began. The term Upper Pleistocene is currently in use as a p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pliocene
The Pliocene ( ; also Pleiocene) is the epoch (geology), epoch in the geologic time scale that extends from 5.33 to 2.58See the 2014 version of the ICS geologic time scale million years ago (Ma). It is the second and most recent epoch of the Neogene Period in the Cenozoic, Cenozoic Era. The Pliocene follows the Miocene Epoch and is followed by the Pleistocene Epoch. Prior to the 2009 revision of the geologic time scale, which placed the four most recent major glaciations entirely within the Pleistocene, the Pliocene also included the Gelasian Stage, which lasted from 2.59 to 1.81 Ma, and is now included in the Pleistocene. As with other older geologic periods, the Stratum, geological strata that define the start and end are well-identified but the exact dates of the start a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Popocatépetl
Popocatépetl ( , , ; ) is an active stratovolcano located in the states of Puebla, Morelos, and Mexico in central Mexico. It lies in the eastern half of the Trans-Mexican Volcanic Belt. At it is the second highest peak in Mexico, after Citlaltépetl (Pico de Orizaba) at . Popocatépetl is ranked 89th by prominence. It is linked to the twin volcano of Iztaccihuatl to the north by the high saddle known as the " Paso de Cortés". Izta-Popo Zoquiapan National Park, wherein the two volcanoes are located, is named after them. Popocatépetl is southeast of Mexico City, from where it can be seen regularly, depending on atmospheric conditions. Until recently, the volcano was one of three tall peaks in Mexico to contain glaciers, the others being Iztaccihuatl and Pico de Orizaba. In the 1990s, the glaciers such as Glaciar Norte (North Glacier) greatly decreased in size, partly due to warmer temperatures but largely due to increased volcanic activity. By early 2001, Popocatép ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratovolcano
A stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high to intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less viscous mafic magma. Extensive felsic lava flows are uncommon, but can travel as far as 8 km (5 mi). The term ''composite volcano'' is used because strata are usually mixed and uneven instead of neat layers. They are among the most common types of volcanoes; more than 700 stratovolcanoes have erupted lava during the Holocene Epoch (the last 11,700 years), and many ol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Río Frío De Juárez
Río Frío de Juárez, originally Río Frío (Cold River), a Mexican populated place, is located in the municipality of Ixtapaluca in the State of Mexico. Río Frío de Juárez is located at the highest point on the highway between Mexico City to Puebla de Zaragoza being located at the top of the pass on the historic road between the two cities. Rio Frio de Juárez, is located near the far eastern border of the State of Mexico, almost on the border of the State of Puebla, at an altitude of 3,000 meters above sea level. It is located on the main roads of the Mexican Federal Highway 150D, Federal Highway 150D and Mexican Federal Highway 190, Mexico-Puebla Highway 190 or Mexico-Puebla Highway. The results of the Census of Population and Housing 2005 conducted by the National Institute of Statistics and Geography state that the total population of Rio Frio is 5,272 and that there are 2,620 men and 2,655 women. History Rio Frio had its origins with the establishment and development o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mexican Federal Highway 150
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Federal Highway 150 (''Carretera Federal 150'') or colloquially called Carretera Puebla - Tehuacan, Carretera Tehuacan - Orizaba, is a Federal Highway of Mexico. The highway travels from Mexico City in the west to Veracruz, Veracruz in the east. Federal Highway 150 is one of five Mexican Federal Highways that terminate in Mexico's capital city. References 150 150 may refer to: * 150 (number), a natural number * AD 150, a year in the 2nd century AD * 150 BC, a year in the 2nd century BC * 150 Regiment RLC * Combined Task Force 150 * 150 Nuwa, a main-belt asteroid * Chevrolet 150, an economy or fleet car ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierra Nevada (Mexico)
The Sierra Nevada ( ) is a mountain range in the Western United States, between the Central Valley of California and the Great Basin. The vast majority of the range lies in the state of California, although the Carson Range spur lies primarily in Nevada. The Sierra Nevada is part of the American Cordillera, an almost continuous chain of mountain ranges that forms the western "backbone" of the Americas. The Sierra runs north-south, and its width ranges from to across east–west. Notable features include the General Sherman Tree, the largest tree in the world by volume; Lake Tahoe, the largest alpine lake in North America; Mount Whitney at , the highest point in the contiguous United States; and Yosemite Valley sculpted by glaciers from one-hundred-million-year-old granite, containing high waterfalls. The Sierra is home to three national parks, twenty-six wilderness areas, ten national forests, and two national monuments. These areas include Yosemite, Sequoia, and Kings Cany ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
