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This document discusses the geomorphology, tectonics, archaeology, and environmental history of the Barrancas locality in central Argentina. The area was located in a distal alluvial plain of an ancient river system that drained eastward. Uplift of nearby mountains starting in the Pliocene redirected river flows, and for most of the Holocene the Barrancas area contained seasonal lakes and lagoons, providing habitat for early human hunter-gatherer populations. Active tectonics and erosion are now dramaticall

Author

iqbal hisham

Language

EN