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The Andes Mountains form a north–south axis of cultural influences. A long series of cultural development culminated in the expansion of the Inca civilization and Inca Empire in the central Andes during the 15th century. The Incas formed this civilization through imperialistic militarism as well as careful and meticulous governmental ...
Simplified sketch of the present-situation along most of the Andes. The Andean orogeny (Spanish: Orogenia andina) is an ongoing process of orogeny that began in the Early Jurassic and is responsible for the rise of the Andes mountains. The orogeny is driven by a reactivation of a long-lived subduction system along the western margin of South ...
The Huancane and Moho groups include red beds and limestone, formed in closed basin. [11] The 1600 kilometer Coastal Batholith of Peru formed in an ensialic marginal basin in the early Cretaceous, with the emplacement of pillow lavas, gabbro and volcaniclastic rocks. In the north, it formed as new continental crust with no older continental ...
In the mountain drainage areas of the Andes, a series of ceremonial buildings were constructed that archaeologists have identified as being a part of what they called the Kotosh Religious Tradition. [18] One of the most prominent of these sites was that at Kotosh, after which the religious tradition was named.
They were closely related to the Muisca people of the Andes, who spoke a Chibcha language. The Timoto-Cuicas were not only composed of the Timoto and the Cuica tribes, but also the Mucuchíes, the Migures, the Tabares, and the Mucuñuques. Timoto-Cuica society was complex with pre-planned permanent villages, surrounded by irrigated, terraced ...
The Andes mountain range as seen from a plane, between Santiago de Chile and Mendoza, Argentina, in summer. The Andes (/ ˈ æ n d iː z / AN-deez), Andes Mountains or Andean Mountain Range (Spanish: Cordillera de los Andes; Quechua: Anti) are the longest continental mountain range in the world, forming a continuous highland along the western edge of South America.
The subduction has formed and continues to form the volcanic Andes Mountain Range. Deformation of the Nazca plate even affects the geography of Bolivia , far to the east (Tinker et al.). The 1994 Bolivia earthquake occurred on the Nazca plate; this had a magnitude of 8.2 M w {\displaystyle M_{w}} , which at that time was the strongest ...
The Andes are generally higher in northern Chile. In Norte Grande the mountains form a series of plateaus, such as Puna de Atacama and the Altiplano.At a south latitude of 27 degrees, Chile's highest mountain (Ojos del Salado) reaches a height of 6,893 metres (22,615 ft).