Late Cenozoic Landforms and Landscape Evolution of Península Valdés

BOUZA, P; BILMES, A.; DEL VALLE, H; ROSTAGNO, C.M.

Late Cenozoic of Península Valdés, Patagonia, Argentina: An Interdisciplinary Approach

Springer

Lugar: Cham; Año: 2017; p. 105 - 129

The present landscape of the Península Valdés is the result of a complex interrelation between climatic (aeolian deposition, windblown processes, glacial and interglacial cycles, pluvial andfluvial processes), tectonic, andeustatic controlsthat had work in the Andean foreland during the late Cenozoic. Based on a geomorphological approach, which includes new descriptions, interpretations, and hierarchically classification of the main landforms of this region, together with previous geomorphological surveys, the Península Valdés area was grouped in three major geomorphologic systems: Uplands and Plains, Great Endorheic Basins, and Coastal Zone. Based on the interrelationship among these three geomorphological systems the landscape evolution of the late Cenozoic of Península Valdés could be summarized infive main stages: (1) development of fluvial and alluvial systems during the Pliocene early Pleistocene; (2) closed basin formation associated to tectonic processes during the early middle Plesitocene; (3)first marine transgressions during the late Pleistocene; (4)flooding of the gulfs and construction of the peninsula in the late Plesitocene?Holocene; (5)final flooding in the region during the middleHolocene.