Fluvial terraces are considered key relief markers to understand environmental changes in the nature time scale, acting as paleo-indicators of morphogenetic processes occurred during the Quaternary, especially the Holocene. ...

This study investigated the lower terrace and floodplain formation in the lower Peixe River in southeastern Brazil. Morphologic, sedimentologic and geochronologic analyses in this meandering tributary of the Parana River ...

The Parana River has been extensively studied in terms of hydrological and sedimentological characterization. However, the geological history of its fluvial plain is poorly understood due the lack of geochronological data. ...

Lithic materials from Lower Palaeolithic are scarce in the Ebro Basin. Archaeological surveys carried out in some alluvial terraces on central Pyrenean piedmont have unearthed three new sites with remains of lithic industries ...

This study, focused on the well-exposed terrace deposits of the Guadalaviar and Turia rivers and associated slopes, provides a better understanding of the genetic connection between river-terrace sediments and slope ...

The aim of this study is to identify and characterize forms and processes associated to the meandering channel pattern in the alluvial valley of the Lower Peixe River, Sao Paulo State, Brazil. Geomorphological interpretations ...

Exposure dating of boulders has been widely applied to determine the age of depositional surfaces under the assumption that the pre-depositional nuclide component in most boulders is negligible. Here we present a case study ...

The lower Gállego River has been strongly degraded since the 1960s due to human activity (gravel mining, dump accumulation, channeling works), which has produced a deep channel incision. Although these human-driven processes ...