The fluvial archive literature is dominated by research on river terraces with appropriate
mention of adjacent environments such as lakes. Despite modern sedimentary basins …

This study documents river terraces from upstream reaches of the Dadès River, a major
fluvial system draining the south-central High Atlas Mountains. Terraces occur as straths …

Regional studies of fluvial landforms and long-term (Quaternary) landscape development in
remote mountain landscapes routinely use satellite-derived DEM data sets. The SRTM and …

Active deformation structures have an incidence in topography that can be quantified by
using geomorphic indices. Most of these indices have been checked in faulted regions with …

Active tectonic deformation influencing the streams and hillslopes of the Sierra Alhamilla
ridge (anticlinorium) in southeast Spain is related to the dextral-reverse Polopos Fault Zone …

One of the challenges facing Earth Scientists is to determine the extent to which geomorphic
features can be used to extract tectonic signals from landscapes. Here, we quantitatively …

Well-constrained case studies of transient landscape responses are needed to improve our
understanding of erosion processes associated with drainage captures. The Duero basin is …

Modern tributary-junction alluvial fans (cone-shaped depositional landforms formed in
confined valley settings) were analysed from a 20-km-long reach of the Dades River in the …

The Duero Basin is one of the largest Cenozoic basins in Iberia and contains a relatively
well-preserved sedimentary infill. The top of the sedimentary sequence crops out at …

The evolution of Cenozoic relief in post-rifted and post-orogenic landscapes reveals
enigmatic and intricate dynamics. Unsteady conditions long after the cessation of ongoing …