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7. Fluvial Landforms (Latin: Fluvius=River)

In humid regions, which receive heavy rainfall running water is considered the most important of the geomorphic agents in bringing about the degradation of the land. The landforms either carved out (due to erosion) or built up (due to deposition) by running water are called Fluvial Landforms (both erosional and depositional) and the running waters which shape them are called fluvial process.

Fluvial processes involve both the overland flow of water down the slope, and stream flow in which water moves in a channel along a valley bottom.

 

7.1. Action of a River/Stream7.1.1. Erosion7.1.2. Transportation7.1.3. DepositionFig: Development of a meander.7.2. River rejuvenation7.2.1. Knick point7.2.2. River Terrace7.2.3. Incised or Entrenched Meanders7.4. Features of Overview8.1.1. Sea Waves mechanismAnatomy of a waveSurf Zone: Swash and Backwash8.2. Coastal erosion8.3. Erosional Features8.3.1. Cliffs and wave-cut-platformsFigure No. 3- Cliff8.3.2. Capes and baysFigure No. 4- Formation of Headlands and Bays8.3.4. Blow holes and GeosFigure No. 6- blow holes8.4.1. Wave-Built Platform or Terrace8.4.2. BeachesBeach and related features8.6. Coastlines of submergence8.7. Coastlines of EmergenceEmergent upland coast