Graded Bedding
This is an old revision of this page, as edited by Iduan (talk | contribs) at 05:16, January 23, 2008. It may differ significantly from current revision.
Graded Bedding is a sedimentary structure where coarser grains gradually give way to finer grains upward through a bed.[1]
Notes
- ↑ Pellant, p. 250
References
- Pellant, Chris. The Complete Book of Rocks and Minerals, Dorling Kindersley Inc.: New York (1995)