Mesoamerica or Meso-America (Spanish: Mesoamérica ) is a region and culture area in the Americas, extending approximately from central Mexico to Honduras and Nicaragua, within which a number of pre-Columbian societies flourished before the Spanish colonization of the Americas in the 15th and 16th centuries.
Prehistoric groups in this area are characterized by agricultural villages and large ceremonial and politico-religious capitals This culture area included some of the most complex and advanced cultures of the Americas, including the Olmec, Teotihuacan, the Maya, and the Aztec.
The term Mesoamerica —literally, "middle America" in Greek—was first used by the German ethnologist Paul Kirchhoff, who noted that similarities existed among the various pre-Columbian cultures within the region that included southern Mexico, Guatemala, Belize, El Salvador, western Honduras, and the Pacific lowlands of Nicaragua and northwestern Costa Rica. In the tradition of cultural-history, the prevalent archaeological theory of the early to middle 20th century, Kirchhoff defined this zone as a culture area based on a suite of interrelated cultural similarities brought about by millennia of inter- and intra-regional interaction (i.e., diffusion).
These included sedentism, agriculture (specifically a reliance on the cultivation of maize), the use of two different calendars (a 260 day ritual calendar and a 365 day calendar based on the solar year), a base 20 (vigesimal) number system, pictographic and hieroglyphic writing systems, the practice of various forms of sacrifice, and a complex of shared ideological concepts. Mesoamerica has also been shown to be a linguistic area defined by a number of grammatical traits that have spread through the area by diffusion.
Mesoamerica is recognized as a near-prototypical cultural area and the term is now fully integrated in the standard terminology of pre-Columbian anthropological studies. Conversely, the sister terms Aridoamerica and Oasisamerica, which refer to northern Mexico and the western United States, respectively, have not entered into widespread usage.
Unrelated to the archaeological and ethnohistorical usage, the term may also be used to refer to a modern economic territory designated the Mesoamerican region (MAR), which comprises the countries of Central America and nine southeastern states of Mexico.
Located on the Middle American isthmus joining North and South America between ca. 10° and 22° northern latitude, Mesoamerica possesses a complex combination of ecological systems, topographic zones, and environmental contexts. Archaeologist and anthropologist Michael D. Coe groups these different niches into two broad categories: the lowlands (those areas between sea level and 1000 meters) and the altiplanos , or highlands (situated between 1000 and 2000 meters above sea level). In the low-lying regions, sub-tropical and tropical climates are most common, as is true for most of the coastline along the Pacific and Gulf of Mexico and the Caribbean Sea. The highlands show much more climatic diversity, ranging from dry tropical to cold mountainous climates, the dominant climate is temperate with warm temperatures and moderate rainfall. The rain fall varies, between the dry Oaxaca, and north Yucatan to the Humid southern Pacific and Caribbean lowlands.
There is extensive topographic variation in Mesoamerica, ranging from the high peaks circumscribing the Valley of Mexico and within the central Sierra Madre mountains to the low flatlands of the northern Yucatán Peninsula. The tallest mountain in Mesoamerica is Pico de Orizaba, a dormant volcano located on the border of Puebla and Veracruz. Its peak elevation is 5,636 m (18,490 ft).
The Sierra Madre mountains, which consist of a number of smaller ranges, run from northern Mesoamerican south through Costa Rica. The chain is historically volcanic. In central and southern Mexico, a portion of the Sierra Madre chain is known as the Eje Volcánico Transversal, or the Trans-Mexican volcanic belt. There are 83 inactive and active volcanoes within the Sierra Madre range, including 11 in Mexico, 37 in Guatemala, 7 in El Salvador, 25 in Nicaragua, and 3 in northwestern Costa Rica. According to the Michigan Technological University , 16 of these are still active. The tallest active volcano is Popocatépetl at 5,452 m (17,883 ft). This volcano, which retains its Nahuatl name, is located 70 km southeast of Mexico City. Other volcanoes of note include Tacana on the Mexico-Guatemala border, Tajumulco and Santamaría in Guatemala, Izalco in El Salvador, Momotombo in Nicaragua, and Arenal in Costa Rica.
One important topographic feature is the Isthmus of Tehuantepec, a low plateau that breaks up the Sierra Madre chain between the Sierra Madre del Sur to the north and the Sierra Madre de Chiapas to the south. At its highest point, the Isthmus is 224 meters (735 ft) above mean sea level. This area also represents the shortest distance between the Gulf of Mexico and the Pacific Ocean in Mexico. The distance between the two coasts is roughly 200 kilometers (120 miles). Although the northern side of the Isthmus is swampy and covered with dense jungle, the Isthmus of Tehuantepec, as the lowest and most level point within the Sierra Madre mountain chain, was nonetheless a main transportation, communication, and economic route within Mesoamerica.
Outside of the northern Maya lowlands, rivers are common throughout Mesoamerica. A number of the more important ones served as loci of human occupation in the area. The longest river in Mesoamerica is the Usumacinta, which forms in Guatemala at the convergence of the Salinas or Chixoy, and La Pasion River and runs north for 970 km (480 km of which are navigable), eventually draining into the Gulf of Mexico. Other rivers of note include the Rio Grande de Santiago, the Grijalva River, the Motagua River, the Ulúa River, and the Hondo River. The northern Maya lowlands, especially the north portion of the Yucatán peninsula, are notable for its nearly complete lack of rivers (largely due to its absolute lack of topographic variation). Additionally, no lakes exist in the northern peninsula. The main source of water in this area, therefore, is sub-surface, and consists of water from aquifers that which is retained within cenotes.
With an area of 8264 km², Lake Nicaragua is the largest lake in Mesoamerica. Lake Chapala is Mexico’s largest freshwater lake, but Lake Texcoco is perhaps the most well-known as the location upon which Tenochtitlan, capital of the Aztec Empire, was founded. Lake Petén Itzá, in northern Guatemala, is notable as the location at which the last independent Maya city, Tayasal (or Noh Petén), held out until 1697. Other large lakes include Lake Atitlán, Lake Izabal, Lake Güija, Lemoa, and Lake Managua.
Almost all ecosystems are present in Mesoamerica; the more well known are the Mesoamerican Barrier Reef System, the second largest in the world, and the Bosawás Biosphere Reserve, a rainforest second in size in the Americas only to the Amazonas. The highlands present mixed and coniferous forest. The biodiversity is among the richest in the world, although the number of species in the red list of the IUCN is growing every year.
There are a number of distinct sub-regions within Mesoamerica that are defined by a convergence of geographic and cultural attributes. These sub-regions are more conceptual than culturally meaningful, and the demarcation of their limits is not rigid. The Maya area, for example, can be divided into two general groups: the lowlands and highlands. The lowlands are further divided into the southern and northern Maya lowlands. The southern Maya lowlands are generally conceptualized as encompassing northern Guatemala, southern Campeche and Quintana Roo in Mexico, and Belize. The northern lowlands cover the remainder of the northern portion of the Yucatán Peninsula. Other areas include Central Mexico, West Mexico, the Gulf Coast Lowlands, Oaxaca, the Southern Pacific Lowlands, and Southeast Mesoamerica (including northern Honduras).
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