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Geomorphology of marine and glacio-lacustrine terraces and raised shorelines in the northern sector of Península Brunswick, Patagonia, Straits of Magellan, Chile

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posted on 2018-03-07, 15:04 authored by Sandro De Muro, Sira Tecchiato, Marco Porta, Carla Buosi, Angelo Ibba

This paper illustrates a detailed geomorphological map (scale 1:50,000) of the marine and transitional terraces (glacio-lacustrine to marine) and raised shorelines linked to Holocene glacio-eustasy and neo-tectonics in the northern area of the Brunswick Penìnsula (Chilean region of the Strait of Magellan). The mapped area is located in Tierra del Fuego between the Segunda Angostura and Seno Otway. This map is the result of geomorphological field survey data integrated with the interpretation of aerial photographs and remote sensing imagery. The survey has allowed the mapping of a sequence of terraces and raised shorelines to be completed. The sequence mainly consists of four orders of marine and glacio-lacustrine terraced deposits, with elevations ranging from 25 to 1 m above mean sea level. The map also presents other landforms and deposits, with their formation linked to littoral, fluvial, glacial and aeolian processes.

Funding

This work was funded through the following sources: (1) Programma Nazionale Ricerche in Antartide (PNRA), ‘Late Quaternary Climatic Evolution in the Magellan-Fuegine area (southern South America)’ and (2) ‘Seismostratigraphy and sedimentology of the South Chile margin’, Supervisor: Antonio Brambati. (3) Regione Autonoma della Sardegna (RAS) – Paesi in Via di Sviluppo (PVS) Project: ‘Coastal geological and geomorphological cartography of Quaternary deposits in the Straits of Magellan (Chile)’, Supervisor: Sandro De Muro. (4) The more recent research project ‘Evolution, dynamics and processes of the coasts and continental shelf in the Mediterranean area and its comparison to other areas on Earth’ (University of Cagliari) finalized the existing cartography (De Muro et al., 2015). Supervisor: Sandro De Muro.

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