The effect of the scale variations applied to the morphometry of the drainage networks is examined in a badland basin, located in the semi-arid Mediterranean area of south-eastern Spain. After a primary statistical analysis, based on the correlation
This paper examines the morphology and temporal development of 4 selected badlands sites (Petrer and Monnegre in Alicante, Vera and Tabernas in Almerιa), paying special attention to the interaction between processes. The study includes two
Comparison and contrast of processes of soil formation in the San Timoteo badlands with chronosequences in California
The purpose of this study is to develop a soil chronology that allows a rigorous correlation of geomorphic surfaces within the San Timoteo Badlands (STB), as well as to nearby surfaces with determined ages at Cajon Pass, Merced, and Anza, to further
. The change in the materials is often accompanied by mass movement activity and the geomorphological consequence is usually the development of badlands topography. It is suggested that by applying the critical state model, a greater consideration can be gained
A comparison of the interrill infiltration, runoff and erosion characteristics of two contrasting badland areas in southern France
Badland ; Drôme ; Erosion des sols ; France ; France du Sud ; Infiltration ; Midi-Pyrénées ; Orage ; Propriétés du sol ; Précipitation ; Rhône-Alpes ; Ruissellement ; Simulation de pluie ; Splash ; Tarn ; Transport sédimentaire ; Versant
Badland ; Drôme ; France ; Infiltration ; Midi-Pyrénées ; Precipitation ; Rainfall simulation ; Rainstorm ; Rhône-Alpes ; Rill wash ; Sediment transport ; Slope ; Soil erosion ; Soil properties ; Southern France ; Splash ; Tarn
Utilisation d'expériences sur petites parcelles pour comparer les caractères de l'infiltration, du ruissellement et de l'érosion dans la zone inter-rigole de 2 régions de badlands du midi de la France: les terres noires des Préalpes françaises et
Dans cette étude des paysages de roubines ou badlands, l'A. tente de préciser le calendrier d'évolution de l'entaille du réseau de torrents secondaires et ravins par l'intermédiaire de l'évolution des profils de ces formes. Il ne s'agit donc pas