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  2. Alluvium (from Latin alluvius, from alluere 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings.
    en.wikipedia.org/wiki/Alluvium
    Alluvial soils are categorized as immature soils. The soil profile is still developing. Alluvial soil has a loamy texture. It is mostly characterized by a blend of sandy and clayey components.
    Alluvium consists of silt, sand, clay, gravel and a good amount of organic matter. The alluvial soils are of recent origin and hence have weak profiles. Alluvial soils have a unique layered look as flood keeps depositing new layers over the earlier one. This process of layering, called stratification, is evident in many floodplains.
    dashamlav.com/alluvial-soils-meaning-characteristi…
    Materials deposited by rivers, winds, glaciers and sea waves are known as alluvium and soils made up of alluvium are alluvial soils. The old alluviums or Bhangar are clayey and sticky, have a darker color, contain nodules of lime concretions and found to lie on slightly elevated lands.
    www.agrifarming.in/crops-suitable-for-alluvial-soil-…
     
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