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  • of scarp retreat rates and internal erosion processes also demonstrated that erosion from rainfall and runoff consistently supplied fine washload sediment in addition to coarse lags of sand bed material. Total sediment yield estimated from empirical
  • washload and theoretical bed material load was dominated by fine washload. A lack of hysteresis in suspended sediment rating curves, scarp retreat and sediment yield correlated to rainfall input, and an equilibrium channel outlet slope supported
  • 2013
  • . Landforms were displayed on geomorphological maps and their evolution was explained in details. The most characteristic landforms on Susak Island are as follows : partly exhumed landforms of the ancient terrain (scarps, limestone cliffs) emerging from loess
  • 2013
  • and perceived origins, have been described. Mantled pediments of etch origin are the most widely distributed and examples now lacking a backing scarp are recognized. Selected Australian regions are considered as possible as examples of pediplains. Areas
  • 2013
  • , patterned ground, debris-covered glaciers and hillslope stripes; and an equatorial assemblage of linked basins, patterned ground, possible pingos, and channel-and-scarp features interpreted to be retrogressive thaw-slumps. Hypotheses to explain
  • 2013
  • , weathering systems. Multi-concave morphology is gradually transformed into multi-convex one, which is hypothesized to be the specific mode of plateau evolution and scarp retreat in granite bedrock.
  • 2013
  • Near-surface airflow over a morphologically simple, vegetated, 8 m high foredune with a small wave-cut scarp was measured for onshore to oblique-onshore conditions during a low-moderate wind event and a high velocity sand-transporting gale event
  • 2013
  • Arid area ; C 14 dating ; Erosion ; Fault scarp ; Geochronology ; Inheritated geomorphological features ; Optically stimulated luminescence ; Palaeo-environment ; Palaeoclimate ; Pyrénées ; Semi-arid area ; Spain ; Talus flatiron
  • 2013