Mesoamerica – meaning "middle of America" – is located in the mid-latitudes (between 10° and 22° N) of the Americas in the southern portion of North America, encompassing much of the isthmus that joins it with South America. Situated within the wider region known as Middle America,[1] Mesoamerica extends from south-central Mexico southeastward to include the Isthmus of Tehuantepec, the Yucatán Peninsula, Guatemala, Belize, El Salvador, and the Pacific coast of Honduras, Nicaragua, and Costa Rica down to the Gulf of Nicoya.
The term Mesoamerica may occasionally refer to the
The region possesses a complex combination of ecological systems. Archaeologist and anthropologist
The highlands of Mesoamerica generally contain two separate regions: the mountainous zone of central and western Mexico, and
Initial hypotheses concerning environmental conditions postulated that the highland climate was more hospitable in the past.[habitats.[citation needed]
The highlands of Mesoamerica, while not extraordinarily rich, Were sufficiently fertile to allow the development of the high agricultural cultures of ancient,
The lowlands, however, offered a great variety of usable flora and fauna resources. These included resources that could not only be consumed in lieu of full-scale agriculture, but also traded to obtain other goods. Furthermore, the greater accessibility of the coast facilitated transportation, interregional communication, and trade.
Mesoamerica as a whole is considered a
Considerable research has been conducted about regional communications in ancient Mesoamerica. There were apparent trade routes starting in the Mexico Central Plateau, and going down to the Pacific coast. These contacts then went on as far as Central America. These trade networks operated with various interruptions from the earliest times and up to the Late Classical Period (600–900 CE).
One of the most important areas in the pre-Columbian history of Mexico is known as 'Central Mexico'. This area is composed of moderate to cold valleys in the southern part of the Mexican high plateau and in the north of the Balsas River basin. It is an ecological niche characterized by its temperate climate and absence of significant water sources. The rains arrive between the months of April and September, and are not abundant. This led to the early development of hydraulic projects, among them the building of canals from the rivers–reservoirs in the hillsides for storing water.
The valley of
The
The climate of the
Unlike the highland regions of central Mexico, the southern Maya highlands are generally cool,
The Fish region has been one of the most diverse since the Mesoamerican epoch. It is a completely mountainous territory, marked by the Sierra Madre del Sur and the Mixteca shield. It includes a portion of the Balsas River basin, characterized by its dryness and complicated geographical relief. Its river beds are shallow and of small capacity. In this sense, it appears much like Central Mexico.
There were two principal scenarios in the cultural history of the Oaxacan people. On the one hand, the central
The other principal scenario was that of the
By the Preclassic period there were already important population centers in the region, such as
Guerrero has traditionally been considered part of Western Mexico. However, recent discoveries have reoriented the divisions of the Mesoamerican cultural areas, and in the works of recent authors, Guerrero is regarded as an independent cultural area. The Guerrero region occupies approximately the area of the southern Mexican state of the same name. It can be divided into three regions with different characteristics: in the north, the Basin of the Balsas River, whose current is the defining characteristic of the regional geography. The Balsas Basin is a low-lying region, with a hot climate and scarce rainfall, whose dryness is mitigated by the presence of the Balsas River and its numerous branches. Central Guerrero corresponds to the Sierra Madre del Sur, a region rich in mineral deposits but poor in agricultural potential. Lastly, the southern part of the region consists of the Pacific coast, a wide coastal plain, full of mangroves and palms, battered by hurricanes from the south.
Guerrero was the site of the first pottery traditions in Mesoamerica. The most ancient remains have been found in Puerto Marqués, near
Western Region is one of the least known areas of Mesoamerica. It is an extensive region that comprises the slopes of the Sierra Madre Occidental, a part of the Sierra Madre del Sur and the middle and lower basin of the Lerma River. The foothills of the mountain were covered by forests of pine and oak, but forestry in the area has reduced its size. The land is suited to cultivation due to its fertility and abundant water resources, especially in the coastal plain of Sinaloa, the Bajío, and the Tarascan Plateau. The climate varies from cold in the mountains, in the east of Michoacán, to tropical along the coast of Nayarit.
This region was inhabited by
The North of Mesoamerica formed part of the cultural super area only during the Classic era (150-750 CE), during which Teotihuacan's apogee, and population growth, favored migration towards the north and commerce with distant Oasisamerica. The region is flat, compressed between the mountain ranges of the Sierra Madre Occidental and the Sierra Madre Oriental. The climate is dry, if not desert-like, with scarce vegetation, for which reason agriculture was only possible through the canalization of surface water currents (especially the Pánuco River and the Lerma tributaries) and the storage of rain water. The excessive dependence on good weather led the people of the North to abandon the region in the middle of the 8th century after enduring a prolonged drought and invasions of Aridoamerican people.
The centers of population in the North were dependent on the network of commerce that was established between Teotihuacan and the Oasis America societies. Sites such as La Quemada in Zacatecas, and La Ferrería in Durango served as forts to guard the commercial routes. When agriculture and the social system collapsed in the North, the occupants of the region migrated towards the West, the Gulf, and the Center of Mexico.
The area known as Centroamerica occupies the Pacific coasts of El Salvador, Honduras, Nicaragua, and the Nicoya Peninsula in Costa Rica. The climate of this region is tropical, with important geological activity, and includes the great Mediterranean lakes of Central America: Lake Nicaragua and Lake Managua. As in the case of the northern region, Centroamerica formed part of the Mesoamerican world only temporarily. It is customary to count the Centroamerican peoples as part of the transition zone between the Andean world and Mesoamerica. Their first contact with the center of Mesoamerica occurred in the Preclassic period, as indicated by the Olmec influence in the area. However, in the Classic period relations were interrupted and Centroamerica received significant cultural influences from the Colombian Altiplano. The development of metallurgy in Centroamerica, for example, occurred much earlier than in the rest of Mesoamerica. During the Postclassic period, the area was again part of the Mesoamerican sphere, as Pipil and Nicarao people, both speakers of Nawat, migrated to this area during the time of the Toltec Empire. Speakers of Subtiaba and Mangue are also thought to have migrated to the area from Mesoamerica proper, though the circumstances of such a migration remain unclear.