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The history of human habitation in the Andean region of South America stretches from circa 15,000 BCE to the present day. Stretching for 7,000 km (4,300 mi) long, the region encompasses mountainous, tropical and desert environments.
The Andean civilizations were South American complex societies of many indigenous people. [1] They stretched down the spine of the Andes for 4,000 km (2,500 miles) from southern Colombia , to Ecuador and Peru , including the deserts of coastal Peru, to north Chile and northwest Argentina .
The Staff God is a major deity of later Andean cultures, and it has been suggested that its use so early points to the worship of common symbols of gods for a long period of time. [10] [11] A view of Caral. Sophisticated government is assumed to have been required to manage the ancient Caral/Norte Chico.
This is a chart of cultural periods of Peru and the Andean Region developed by John Rowe and Edward Lanning and used by some archaeologists studying the area. An alternative dating system was developed by Luis Lumbreras and provides different dates for some archaeological finds.
Scientists explain the loss of the Humboldt Glacier in Venezuela's Sierra Nevada, which they believe makes the South American country the first in modern history to lose all its glaciers.
The history of South America is the study of the past, particularly the written record, oral histories, and traditions, passed down from generation to generation on the continent of South America. The continent continues to be home to indigenous peoples, some of whom built high civilizations prior to the arrival of Europeans in the late 1400s ...
Although the Andean population was devastated by the internal wars of Spaniards and Incas, the ravages of European diseases, and forced, brutal labor in silver and mercury mines, the Andean Indian cultures remained in many ways little changed from the days when the Incas ruled. [3] By the late 1560s, Spanish rule of the Andes was in crisis.
Map of a north-south sea-parallel pattern of rock ages in western Colombia. This pattern is a result of the Andean orogeny. Tectonic blocks of continental crust that had separated from northwestern South America in the Jurassic re-joined the continent in the Late Cretaceous by colliding obliquely with it. [6]