Lake Texcoco
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Lake Texcoco | |
---|---|
Lago de Texcoco Tetzco(h)co | |
paleo lake | |
Surface area | 2,100 square miles (5,400 km2) |
Max. depth | over 500 feet (150 m) |
Surface elevation | 7,349 feet (2,240 m) |
Official name | Lago de Texcoco |
Designated | 5 June 2022 |
Reference no. | 2469[1] |
Lake Texcoco (
The entire lake basin is now almost completely occupied by
After the cancellation of the Mexico City Texcoco Airport, the government initiated a major restoration project of a significant part of the lake in the form of the Lake Texcoco Ecological Park, 14,000 hectares of public space and ecological restoration.
Geography
The
History
Between the
Agriculture around the lake began about 7,000 years ago,[6] with humans following the patterns of periodic inundations of the lake.
Several villages appeared on the northeast side of the lake between 1700 and 1250 BC. By 1250 BC the identifying signs of the Tlatilco culture, including more complex settlements and a stratified social structure, are seen around the lake. By roughly 800 BC Cuicuilco had eclipsed the Tlatilco cultural centers and was the major power in the Valley of Mexico during the next 200 years when its famous conical pyramid was built. The Xitle volcano destroyed Cuicuilco around AD 30, a destruction that may have given rise to Teotihuacan.
After the fall of Teotihuacan, AD 600–800, several other city states appeared around the lake, including Xoloc, Azcapotzalco, Tlacopan, Coyohuacan, Culhuacán, Chimalpa, and Chimalhuacán – mainly from Toltec and Chichimeca influence. None of these predominated and they coexisted more or less in peace for several centuries. This time was described as a Golden age in Aztec chronicles. By the year 1300, however, the Tepanec from Azcapotzalco were beginning to dominate the area.
Tenochtitlan
According to a traditional story, the Mexica wandered in the deserts of modern Mexico for 100 years before they came to the thick forests of the place now called the Valley of Mexico.
The Aztec ruler Ahuitzotl attempted to build an aqueduct that would take fresh water from the mainland to the lakes surrounding the Tenochtitlan city. The aqueduct failed, and the city suffered a major flood in 1502.[8][9]
During Hernán Cortés's siege of Tenochtitlan in 1521, the dams were destroyed, and never rebuilt, so flooding became a big problem for the new Mexico City built over Tenochtitlan.
Artificial drainage
Mexico City suffered from periodic floods; in 1604 the lake flooded the city, with an even more severe flood following in 1607. Under the direction of Enrico Martínez, a drain was built to control the level of the lake, but in 1629 another flood kept most of the city covered for five years. At that time, it was debated whether to relocate the city, but the Spanish authorities decided to keep the existing location.[citation needed]
Eventually the lake was drained by the channels and a tunnel to the Pánuco River, but even that could not stop floods, since by then most of the city was under the water table. The flooding could not be completely controlled until the twentieth century. In 1967, construction of the Drenaje Profundo ("Deep Drainage System"), a network of several hundred kilometers of tunnels, was done, at a depth between 30 and 250 m (98 and 820 ft). The central tunnel has a diameter of 6.5 m (21.3 ft) and carries rain water out of the basin. The eastern discharge tunnel was inaugurated in 2019.[citation needed]
The ecological consequences of the draining were enormous. Parts of the valleys were turned semi-arid, and even today Mexico City suffers from lack of water. Due to overdrafting that is depleting the aquifer beneath the city, Mexico City is estimated to have sunk 10 meters (33 feet) in the last century.[10] Furthermore, because soft lake sediments underlie most of Mexico City, the city has proven vulnerable to soil liquefaction during earthquakes, most notably in the 1985 earthquake when hundreds of buildings collapsed and thousands of people died.[11]
The term "Texcoco Lake" now refers only to a big area surrounded by salt marshes 4 km (2.5 mi) east of Mexico City, which covers part of the ancient lake bed. Also there are small remnants of the lakes of Xochimilco, Chalco, and Zumpango.[citation needed]
Several species indigenous to the lake are now extinct or endangered (e.g. axolotls).[12]
The modern Texcoco Lake has a high concentration of salts and its waters are evaporated for their processing. A Mexican company, "Sosa Texcoco S.A." has an 800-hectare (2,000-acre) solar evaporator known as El Caracol.[citation needed]
Land reclamation of the lakebed was part of Mexico's attempts at development in the twentieth century.[13]
Restoration and conservation
Ecological park
The Lake Texcoco Ecological Park, officially called Parque Ecológico Lago de Texcoco (PELT),[14] is a project of the government of Mexico which consists of an urban park in the State of Mexico. It is part of the larger metropolitan area in the Valley of Mexico, around Mexico City.[15]
The planned area for the park is 14,000 ha (35,000 acres),[16] of which 4,800 ha (12,000 acres) will be public spaces.[15] The government has announced that the park will open of 30 April 2024.[16][17] The park was designated after the cancelling of an airport in the same location.
The park has been internationally praised as both a major ecological restoration project, and having great potential for climate adaptation for Mexico City.[18][19]See also
- History of Mexico City
- Index of Mexico-related articles
- Paleontological Museum in Tocuila
- List of prehistoric lakes
Notes
- ^ "Lago de Texcoco". Ramsar Sites Information Service. Retrieved 5 November 2022.
- ^ Jones, Benji (2022-01-25). "The animal that's everywhere and nowhere". Vox. Retrieved 2023-12-12.
- S2CID 162952844.
- S2CID 140202319. Retrieved 2016-10-03.
- ^ Siebe et al. (1999)
- ^ Niederberger (1979)
- ISBN 978-0-918334-80-0.
- ISBN 978-0-8061-2679-1.
- ^ "Moctezuma: The leader who lost an empire". 2009-09-21.
- ^ Sample, Ian. "Why is Mexico City sinking?". The Guardian. Retrieved 3 October 2016.
- ISSN 0121-2974.
- ^ Jones, Benji (2022-01-25). "The animal that's everywhere and nowhere". Vox. Retrieved 2023-12-12.
- ^ Matthew Vitz, "'The Land with which we struggle': Land Reclamation, Revolution, and Development in Mexico's Lake Texcoco Basin, 1910-1950". Hispanic American Historical Review 92, no. 1 (2012): 41-71.
- ^ SEMARNART. "Proyecto ecológico Lago de Texoco" (PDF). Retrieved 26 June 2021.
- ^ a b "Gobierno de AMLO presenta proyecto de Parque Ecológico para rescatar Lago de Texcoco". Forbes. Retrieved 25 June 2021.
- ^ a b "Así será el Parque Ecológico del Lago de Texcoco". Retrieved 15 June 2022.
- ^ https://diarioportal.com/2024/01/17/con-81-de-avance-conagua-estima-apertura-del-parque-ecologico-lago-de-texcoco-en-abril-2/
- ^ "Mexico City is proposing to build one of the world's largest urban parks. Will it serve as a climate adaptation example for other cities?". Ensia. Retrieved 2021-10-03.
- ^ "Will Mexico City's massive new park be a climate adaptation paragon for other cities? | Greenbiz". www.greenbiz.com. Retrieved 2021-10-03.
References
- Agostini, Claudia (2003). Monuments of Progress: Modernization and Public Health in Mexico City, 1876–1910. Latin American and Caribbean series, no. 4. Calgary and Boulder: OCLC 51495264.
- Aréchiga Córdoba, Ernesto (July–August 2004). "El desagüe del Valle de México, siglos XVI–XXI: Una historia paradójica" (PDF). online reproduction) on 2008-05-15.
- Arroyo-Cabrales, Joaquín; Elaine Johnston; Luis Morett A. (2001). "Mammoth bone technology at Tocuila in the Basin of Mexico". In G. Cavarretta; P. Gioia; M. Mussi; M.R. Palombo (eds.). La Terra degli Elefanti: atti del 1o Congresso Internazionale = The World of Elephants: proceedings of the 1st International Congress. 1st International Congress "the World of Elephants", Rome, 16–20 October 2001. Rome: online reproduction) on 6 June 2008.
- OCLC 27035231.
- Bradbury, John P. (March 1971). "Paleolimnology of Lake Texcoco, Mexico. Evidence from Diatoms". Limnology and Oceanography. 16 (2): 180–200. OCLC 1715910.
- OCLC 162351797.
- Joint Academies Committee on the Mexico City Water Supply (1995). Mexico City's Water Supply: Improving the Outlook for Sustainability (published online). with the participation of the Water Science and Technology Board, Commission on Geosciences, Environment, and Resources, OCLC 42330470. (in English and Spanish)
- S2CID 29625197.
- online reproduction) on 2008-05-11.
- Siebe, Claus; Peter Schaaf; Jaime Urrutia-Fucugauchi (October 1999). "Mammoth bones embedded in a late Pleistocene lahar from Popocatépetl volcano, near Tocuila, central México". Geological Society of America Bulletin. 111 (10): 1550–1562. OCLC 94209925.
External links
- Agua y Subordinación en la Cuenca del Río Lerma (in Spanish)