Celaya | Mexico
There are many smaller towns around Celaya including Rincón de Tamayo, Tarimoro, Salvatierra, La Moncada, Panales Jamaica (Cañones), Panales Galera, La Calera, La Estancia, La Noria, La Acebuche, Cacalote, and Charco Largo.
Universidad de Itesba
Universidad Latina de Mexico
Universidad Lasallista Benavente
Universidad de Celaya
Instituto Tecnologico de Celaya
Instituto Tecnologico de Roque
Escuela Bilingue Guilford
Colegio Arturo Rosenblueth
Westminster Royal College
Tecnologico de Monterrey
The work was carried out under the command of German Enrique Schöndube, although it is known that payment for the construction took ten years due to the start of the Mexican Revolution, so it was paid once the new government established. During the Mexican Revolution, Villa's officers thought the hydraulic tower had such a large amount of water that destroying it would drown the population of Celaya. One of Villa's generals ordered his artillery to destroy it. Captain Gustavo Duron, in charge of a 75mm battery, followed the orders but shot around the tower, avoiding it and protecting the monument, as mentioned by local historian Herminio Martínez. The construction resulted in the neglect of the people handing out water at home from the mayor's office called water carriers. Commercial advertising on its surface was allowed for several years to cover the costs of the reservoir, ending on September 8, 1980 when, in celebration of upcoming 410th Anniversary of the Foundation of Celaya, the mayor in charge decreed that the Ball of Water would be a symbol that would represent the city, and the placement of advertisements was banned.
Climates in the state are grouped by precipitation and average temperatures into three major groups. The semi-arid climate is characterized by the fact that evaporation often exceeds precipitation. Most of the vegetation in these areas is arid grassland with desert plants such as nopal. These climates cover about forty percent of the state, mostly in the north. Semi-arid temperate regions are found in the municipalities of San Felipe, San Diego de la Unión, San Luis de la Paz, part of Dolores Hidalgo and San José de Iturbide, where precipitation varies between 400 and 500 mm and the average temperature is between 16 and 18 °C. Semi-arid semi hot climates can be found north of Dolores Hidalgo, around León and in areas near Celaya. In these municipalities, rainfall averages between 600 and 700 mm and the average annual temperature is between 18 and 20 °C. Temperate climates are judged by the presence of holm oak and pine forest, pine forests and/or pine forests with meadows. Humidity varies in these forest regions. Temperate semi-moist areas are mostly found in the southeast municipalities of Apaseo, Coroneo and Jerécuaro and in the center of the state. Precipitation varies from 600 to 700 mm and the average temperature is between 16 and 18 °C. Temperate and somewhat humid climates have rainfall averages of between 700 and 800 mm, with temperatures between 16 and 18 °C. These can be found in Pénjamo, Coroneo, Jerécuaro and parts of Guanajuato (municipality) and Dolores Hidalgo. Temperate climates with the most humidity are found in the Santa Rosa and municipality of Guanajuato. These have rainfall averages of over 800 mm and average temperatures of under 16 °C. Hot and moist climates in the state have temperatures ranging from 18 to 22 °C and are associated with tropical rainforest, with some grassland. These climates are subdivided into two types, one that receives less rainfall with a significant dry season and the other which is wetter. The drier type is found in Abasolo, Irapuato, Salamanca and Romita. In total, these hot and relatively moist climates can be found in about 40% of the state.
In 1590, the Villa de San Luis de la Paz was founded named after the peace (paz) treaty between the Spanish and the Chichimeca. With the Spanish occupying most of the most productive land and its resources, the indigenous of the area became extremely impoverished. This eventually allowed the Spanish to negotiate peace with chiefs in exchange for basic goods such as blankets, clothes and food. This would bring temporary truces. For the long term, evangelization efforts would bring longer term submission. Franciscans and Augustinians worked to gradually modify the worldview of the Chichimecas and others until many moved out of the mountains and into settlements and profess, at least nominally, the Catholic faith. However, the indigenous remained extremely marginalized and poor, losing both language and culture until most eventually intermarried with outsiders to produce mestizos. Through the colonial period, most of the area's wealth came from mining, with much of the agriculture springing up to support the mining communities. The height of mining came in the 18th century, mostly from the mines in the hills around the city of Guanajuato, leading to the construction of a large number of notable civil and religious buildings in the same area. The Bajío area was extremely fertile and became a major agricultural area for New Spain. Both of these activities brought in more Spanish and Criollos to take advantage, as well as mestizos and some African slaves to work the mines and fields, making the area's population grow rapidly and eventually concentrate in urban centers. The area was made an "indentencia" or province in 1786, when New Spain was divided into twelve parts.