Plain Course Of A River
A plain is a flat, low-lying area of land that has been formed over time by the gradual accumulation of sediment from bodies of water such as rivers and streams. Plains are often associated with a general lack of variation in elevation, but in reality, they can rise to considerable heights, depending on the nature of the underlying bedrock. In the context of rivers, plain river courses tend to be relatively wide, shallow and meandering. This is usually a result of uniform deposition of sediment throughout the length of the watercourse, resulting in a slow, steady decrease in the energy of the flow. As the current weakens it is more easily deflected by the wind and the surface of the water itself, resulting in broad meander bends. In addition to their wide, shallow, meandering nature, plain river courses are characterised by the presence of floodplains. These are areas of flat, low-lying land which are prone to flooding when the flow of a river increases. Floodplains often contain highly fertile soils, making them important areas for agricultural use. Plain river courses are generally slow-moving and appear very calm. This is because the steady rate of sediment deposition throughout the watercourse has resulted in a near-constant depth and rate of flow throughout its length. This stability in the watercourse encourages the growth of aquatic vegetation along its banks, which may also add to its apparent calmness.
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