• Author: Stokes, M.

    University of Plymouth, United Kingdom

  • Author: Mather, A.E.

    University of Plymouth, United Kingdom

  • Author: Belfoul, M.

    Universite Ibn Zohr, Morocco

  • Author: Faik, F.

    Universite Ibn Zohr, Morocco

  • Author: Bouzid, S.

    Universite Ibn Zohr, Morocco

  • Author: Geach, M.R.

    University of Plymouth, United Kingdom

  • Author: Cunha, P. P.

    Universidade de Coimbra, Portugal

  • Author: Boulton, Simon J.

    University of Plymouth, United Kingdom

  • Author: Thiel, Christine

    Center for Nuclear Technologies, Technical University of Denmark, Frederiksborgvej 399, 4000, Roskilde, Denmark

View graph of relations

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 with bedrock bases positioned at 10 m altitudinal intervals up to 40 m (T1-T5) above the valley floor, becoming less common between 50 and 140 m. The rock strength, stratigraphy and structure of the mountain belt influences terrace distribution. Terraces are absent in river gorges of structurally thickened limestone; whilst well-developed, laterally continuous terraces (T1-T4) form along wide valleys occupying syncline structures dominated by weaker interbedded limestone-mudstone. Terrace staircases develop in confined canyons associated with weaker lithologies and influence from structural dip and stratigraphic configuration. Terraces comprise a bedrock erosion surface overlain by fluvial conglomerates, rare overbank sands and colluvium. This sequence with some OSL/IRSL age control, suggests terrace formation over a 100 ka climate cycle with valley floor aggradation during full glacials and incision during glacial-interglacial transitions. This integrates with other archives (e.g. lakes, glaciers, dunes), appearing typical of landscape development along the NW Saharan margin south of the High Atlas, and similar to patterns in the western-southern Mediterranean. The 100 ka climate cycle relationship suggests that the terrace sequence documents Late-Middle Pleistocene landscape development. Consistent altitudinal spacing of terraces and their distribution throughout the orogen suggests sustained base-level lowering linked to uplift-exhumation of the High Atlas. Low incision rates (<0.2 mm a-1) and general absence of terrace deformation suggests dominance of isostatically driven base-level lowering with relief generation being Early Pleistocene or older.
Original languageEnglish
JournalQuaternary Science Reviews
Pages (from-to)363-379
Number of pages17
Publication statusPublished - 2017
CitationsWeb of Science® Times Cited: No match on DOI

    Research areas

  • Africa, Climate dynamics, Fluvial geomorphology, Optical methods, Paleogeography, Pleistocene

Download statistics

No data available

ID: 133577783