Geomorphology and internal architecture of Holocene sandy-gravel beach ridge plain and barrier spits at Río Chico area, Tierra del Fuego, Argentina

MONTES, ALEJANDRO; BUJALESKY, GUSTAVO; PAREDES, JOSÉ MATILDO

JOURNAL OF SOUTH AMERICAN EARTH SCIENCES

PERGAMON-ELSEVIER SCIENCE LTD

Año: 2018 p. 172 - 183

0895-9811

The internal architecture and processes involved in the development of paraglacial sandy-gravel beach ridges and barrier spits have been analyzed by interpretation of ground-penetrating radar (GPR) records, satellite images and detailed topographicalsections on Holocene deposits in Río Chico area, Tierra del Fuego, Argentina. These littoral deposits correspond to the infill of an extensive and shallow embayment facing the South Atlantic, and developed during the mid-Holocene. Radar facies wereidentified and characterized from both beach ridge plain and barrier spits. The radar facies in the beach ridge plain are interpreted as mainly progradational and regressive, associated with stages of high availability of sediment supply. On the contrary, barrierspits show a retrogradational pattern and occurred in transgressive conditions by rollover processes during periods of marked scarcity of sediment supply. Evolutionary models of the internal architecture of both beach ridge plain and barrier spits are developedfor the southern hemisphere during stable sea level conditions.