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In [[sedimentary rock]], when all the grains are much the same size.
 
In [[sedimentary rock]], when all the grains are much the same size.
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Pellant, p. 251
      
=Sources=
 
=Sources=
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*Pellant, Chris. ''The Complete Book of Rocks and Minerals'', Dorling Kindersley Inc.: New York (1995)
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*Pellant, Chris. ''The Complete Book of Rocks and Minerals'', Dorling Kindersley Inc.: New York (1995), p. 251
    
[[category:geology]]
 
[[category:geology]]
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