Fluvial Desert Landforms: Shaped by Water in Arid Regions

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Fluvial Desert Landforms

Running water plays a significant role in shaping landscapes, particularly in semi-arid regions that experience moderate rainfall.

Fluvial Desert Landforms

  • Washes/Wadis: These are valley-like ravines, often characterized by interlocking spurs.
  • Badlands: When a surface is heavily dissected by numerous wadis, it results in a distinctive topography known as Badlands.
    • Example: The Chambal Badlands in India. 
  • Mesas and Buttes: In arid plateaus, when a resistant horizontal layer is eroded by wind and water, it forms mesas and buttes.
    • Mesas: Flat-topped, steep-sided landforms separated from the main plateau.
    • Buttes: Smaller versions of mesas.
  • Bolsons: These are intermontane basins found in arid and semi-arid regions.
  • Playas: Temporary lakes that form in the center of bolsons where water accumulates.
    • Example: Lake Lop Nor in the Tarim Basin, northwest China.
  • Pediments: Broad, gently sloping rock-cut surfaces located between a mountain front and the adjacent bajada.
  • Bajada: A gently sloping depositional plain that lies between pediments and playas.
    • Formed by the merging of several alluvial fans.

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