Sorting (sediment)

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Sediment consisting of well sorted grains (left) compared with poorly sorted grains (right).

Sorting describes the distribution of grain size of sediments, either in unconsolidated deposits or in sedimentary rocks. This should not be confused with crystallite size, which refers to the individual size of a crystal in a solid. Crystallite is the building block of a grain. Very poorly sorted indicates that the sediment sizes are mixed (large variance); whereas well sorted indicates that the sediment sizes are similar (low variance).

The terms describing sorting in sediments – very poorly sorted, poorly sorted, moderately sorted, well sorted, very well sorted – have technical definitions and semi-quantitatively describe the amount of variance seen in particle sizes. See Grain size § Sorting for details. In the field, sedimentologists use graphical charts to accurately describe the sorting of a sediment using one of these terms.[1]

The degree of sorting may also indicate the energy, rate, and/or duration of deposition, as well as the transport process (river, debris flow, wind, glacier, etc.) responsible for laying down the sediment. Sorting of sediments can also be affected by reworking of the material after deposition, for instance, by winnowing.[2]

Rocks derived from well sorted sediments are commonly both porous and permeable, while poorly sorted rocks have low porosity and low permeability, particularly when fine grained.

See also[edit]


  1. ^ Tucker, M.E., 1996, Sedimentary rocks in the field, John Wiley & Sons, Chichester, 153 p.
  2. ^ Compton, R. R., 1962, Manual of field geology, John Wiley & Sons, 378 p.