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Sierra De Las Cruces
The Sierra de las Cruces, also popularly called Sierra del Monte de las Cruces, is a mountain range in Mexico, in its south central region, which delimits the valleys of Mexico and Cuautitlán in the Basin of Mexico, with Toluca Valley as well as a part of the Lerma Basin. The Battle of Monte de las Cruces took place in this mountain range, as well as the construction of the Cutzamala System. It is part of the Transversal Volcanic Axis, and represents the watershed of three hydrological basins: the Lerma River, the Valley of Mexico (both of the endorheic type) and the Balsas River (of the exorheic type). History Due to the studies carried out in the mountains, it is considered that Sierra de las Cruces was formed next to the Trans-Mexican Volcanic Belt, which is considered a continental volcanic arc, formed since the recent Miocene epoch, with the La Catedral stratovolcano being the oldest with about 3.71 ± 0.40 million years. years., with an important activity during the Pliocene ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Toluca Valley
The Toluca Valley is a valley in central Mexico, just west of the Valley of Mexico (Mexico City), the old name was Matlatzinco. The valley runs north–south for about , surrounded by mountains, the most imposing of which is the Nevado de Toluca Volcano. It is one of the highest valleys in Mexico and for this reason has a relatively cold climate. Since the 1940s, there has been significant environmental degradation in the valley, with the loss of forests, soil erosion, falling water tables and water pollution due to growth in industry and population. In the pre-Hispanic period, it was a buffer region between the Aztec Empire and Purépecha Empire. From the Aztec period until the 19th century, it was part of the region controlled by Mexico City, but today it is the center of the State of Mexico, which has its capital in Toluca, the main city of the valley. Physical geography and climate The Toluca Valley is a broad highland valley located immediately west of the Valley of Mexico. I ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Battle Of Monte De Las Cruces
The Battle of Monte de las Cruces was one of the pivotal battles of the early Mexican War of Independence, in October 1810. It was fought between the insurgent troops of Miguel Hidalgo y Costilla and Ignacio Allende against the New Spain royalist troops of Lt Colonel Torcuato Trujillo, in the Sierra de las Cruces mountains between Toluca and Mexico City. The battle marks the furthest advance of the first rebel campaign, before Hidalgo decided to retreat towards Guadalajara, and not attack Mexico City, despite the fact that he won the battle, but at high cost. The battlefield is now located in the La Marquesa National Park, which is officially called the Miguel Hidalgo National Park in honor of the event. Grito de Dolores and march to the Sierra de las Cruces The battle marks the end of the first offensive in the Mexican War of Independence, which began with the Grito de Dolores. Father Miguel Hidalgo y Costilla was the parish priest of Dolores, Guanajuato, involved with one of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lerma River
The Lerma River ( es, Río Lerma) is Mexico's second longest river. It is a river in west-central Mexico that begins in Mexican Plateau at an altitude over above sea level, and ends where it empties into Lake Chapala, Mexico's largest lake, near Guadalajara, Jalisco. Lake Chapala is the starting point of Río Grande de Santiago, which some treat as a continuation of the Lerma River. In combination, the two are often called the Lerma Santiago River ( es, Río Lerma Santiago). The Lerma River is notorious for its pollution, but the water quality has demonstrated considerable improvement in recent years due mostly to government environmental programs and through massive upgrading projects of sanitation works. Course The Lerma River originates from the Lerma lagoons near Almoloya del Río, on a plateau more than above sea level, and southeast of Toluca. The lagoons receive their water from springs rising from basaltic volcanics that flow down from Monte de Las Cruces. These are lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley Of Mexico
The Valley of Mexico ( es, Valle de México) is a highlands plateau in central Mexico roughly coterminous with present-day Mexico City and the eastern half of the State of Mexico. Surrounded by mountains and volcanoes, the Valley of Mexico was a centre for several pre-Columbian civilizations, including Teotihuacan, the Toltec, and the Aztec. The ancient Aztec term ('Land Between the Waters') and the phrase Basin of Mexico are both used at times to refer to the Valley of Mexico. The Basin of Mexico became a well known site that epitomized the scene of early Classic Mesoamerican cultural development as well. The Valley of Mexico is located in the Trans-Mexican Volcanic Belt. The valley contains most of the Greater Mexico City, Mexico City Metropolitan Area, as well as parts of the State of Mexico, Hidalgo (state), Hidalgo, Tlaxcala, and Puebla. The Basin of Mexico covers approximately in the NNE-SSW direction with length to width dimensions of approximately to The Valley of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trans-Mexican Volcanic Belt
The Trans-Mexican Volcanic Belt ( es, Eje Volcánico Transversal), also known as the Transvolcanic Belt and locally as the (''Snowy Mountain Range''), is an active volcanic belt that covers central-southern Mexico. Several of its highest peaks have snow all year long, and during clear weather, they are visible to a large percentage of those who live on the many high plateaus from which these volcanoes rise. History The Trans-Mexican Volcanic Belt spans across Central-Southern Mexico from the Pacific Ocean to the Gulf of Mexico between 18°30'N and 21°30'N, resting on the southern edge of the North American Plate. This approximately 1000 kilometer long, 90–230 km broad structure is an east–west, active, continental volcanic arc; encompassing an area of approximately 160,000 km2. Over several million years, the subduction of the Rivera and Cocos plates beneath the North American Plate along the northern end of the Middle America Trench formed the Trans-Mexican Vol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tepoztlán
Tepoztlán () is a town in the central Mexican state of Morelos. It is located at in the heart of the Tepoztlán Valley. The town serves as the seat of government for the municipality of the same name. The town had a population of 14,130 inhabitants, while the municipality reported 41,629 inhabitants in the 2010 national census. The town is a popular tourist destination near Mexico City. The town is famous for the remains of El Tepozteco temple built on top of the nearby Tepozteco Mountain, as well as for the exotic ice cream flavors prepared by the townspeople. Tepoztlán was named a "Pueblos Mágicos (Mexico), Pueblo Mágico" (or ''magic town'') in 2002 but its title was removed in 2009 for failure to maintain the requirements. In 2010 Tepoztlán addressed these problems and recovered the Pueblo Mágico title. Etymology Tepoztlán is derived from Nahuatl and means "place of abundant copper" or "place of the broken rocks." This is derived from the words ''tepoz-tli'' (copper) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierra De Guadalupe, Mexico
The Sierra de Guadalupe is a mountain range in Mexico. It is found between the borough of Gustavo A. Madero in northern Mexico City and the municipalities of Cuautitlán Izcalli, Tultitlán, Coacalco, Ecatepec and Tlalnepantla, in the State of Mexico. Its highest peak is at . History There is evidence that the Aztecs worshipped Tonantzin (Goddess of Sustenance) at Tepeyac hill. The sierra is named after Our Lady of Guadalupe, a Marian apparition that, according to oral and written colonial sources such as the ''Huei tlamahuiçoltica'', Juan Diego saw at the Tepeyac hill. In 1937, the El Tepeyac National Park was created in the Tepeyac hill, in the eastern portion of the sierra, by decree of the president Lázaro Cárdenas. Geology The sierra is a dormant volcano that is part of the Trans-Mexican Volcanic Belt. The basement is made of andesitic and dacitic soil. The last volcanic activity in the area occurred 14 to 15 million years ago. Ecology Climate The sierra ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Mexico
The geography of Mexico describes the geographic features of Mexico, a country in the Americas. Mexico is located at about 23° N and 102° W in the southern portion of North America. From its farthest land points, Mexico is a little over in length. Mexico is bounded to the north by the United States (specifically, from west to east, by California, Arizona, New Mexico, and Texas), to the west and south by the Pacific Ocean, to the east by the Gulf of Mexico, and to the southeast by Belize, Guatemala, and the Caribbean Sea. The northernmost constituent of Latin America, it is the most populous Spanish-speaking country in the world. Mexico is the world's 13th largest country, three times the size of Texas. Almost all of Mexico is on the North American Plate, with small parts of the Baja California Peninsula in the northwest on the Pacific and Cocos Plates. Some geographers include the portion east of the Isthmus of Tehuantepec including the Yucatán Peninsula within North Amer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Mexico City
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of The State Of Mexico
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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