Geomorphologic and stratigraphic studies accomplished in the littoral area between Cabo Raso and Punta Fabián, eastern Chubut Province, allowed the identification of different features and geomorphologic processes related to the modern dinamic, as well as a set of coastal units related to the different transgressive events occurred from the middle Pleistocene to the Holocene. The distribution and development of the littoral deposits displays a completely different situation from that of the area of Bahía Camarones, Bahía Bustamante, Cabo Raso and Bahía Vera (south and north of the study area), favored by a very hard substrate (Marifil Complex) at higher topographic positions. Abrasion platforms, cliffs, islands, capes and tómbolos form a br...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
This paper presents a 1:100,000 scale geomorphologic map of the Northeastern sector of San Jorge Gul...
The internal architecture and processes involved in the development of paraglacial sandy-gravel beac...
The stratigraphic reconstruction of the northern sector of theBahía Camarones (Chubut, Argentina) al...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Provinc...
The stratigraphic reconstruction of the northern sector of the Bahía Camarones (Chubut, Argentina...
Morphological characteristics of Ameghino isthmus, Chubut province, Argentina, are described. Spatia...
The stratigraphic reconstruction of the northern sector of the Bahía Camarones (Chubut, Argentina) a...
The Holocene evolution of the Cabo Raso bay (Atlantic Patagonian coast) was reconstructed by means o...
A description and genetic analysis of themorphological units present in the northwestern coastal are...
Holocene coastal environments in the Tierra del Fuego archipelago in southernmost South America evol...
Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Provinc...
The Patagonian coast evolved in relation to different issues. An arid climate dominates to the north...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
This paper presents a 1:100,000 scale geomorphologic map of the Northeastern sector of San Jorge Gul...
The internal architecture and processes involved in the development of paraglacial sandy-gravel beac...
The stratigraphic reconstruction of the northern sector of theBahía Camarones (Chubut, Argentina) al...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
The coastal fringe of Central Patagonia preserves a unique and spectacular succession of landforms d...
Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Provinc...
The stratigraphic reconstruction of the northern sector of the Bahía Camarones (Chubut, Argentina...
Morphological characteristics of Ameghino isthmus, Chubut province, Argentina, are described. Spatia...
The stratigraphic reconstruction of the northern sector of the Bahía Camarones (Chubut, Argentina) a...
The Holocene evolution of the Cabo Raso bay (Atlantic Patagonian coast) was reconstructed by means o...
A description and genetic analysis of themorphological units present in the northwestern coastal are...
Holocene coastal environments in the Tierra del Fuego archipelago in southernmost South America evol...
Stratigraphic, morphologic and radiocarbon data from Puerto Deseado coastal area (Santa Cruz Provinc...
The Patagonian coast evolved in relation to different issues. An arid climate dominates to the north...
This paper concerns the relative sea-level changes associated with the Atlantic Patagonian coast der...
This paper presents a 1:100,000 scale geomorphologic map of the Northeastern sector of San Jorge Gul...
The internal architecture and processes involved in the development of paraglacial sandy-gravel beac...