Difference between revisions of "Graded Bedding"
Jump to navigation
Jump to search
Liam Spencer (talk | contribs) m (Minor addition.) |
(major format) |
||
| Line 1: | Line 1: | ||
| − | '''Graded Bedding''' is a [[Sedimentary rock|sedimentary]] structure where coarser grains gradually give way to finer grains upward through a bed. | + | '''Graded Bedding''' is a [[Sedimentary rock|sedimentary]] structure where coarser grains gradually give way to finer grains upward through a bed.<ref>Pellant, p. 250</ref> |
| − | + | ==Notes== | |
| − | Pellant, p. 250 | + | {{reflist}} |
| − | + | ==References== | |
| − | = | ||
*Pellant, Chris. ''The Complete Book of Rocks and Minerals'', Dorling Kindersley Inc.: New York (1995) | *Pellant, Chris. ''The Complete Book of Rocks and Minerals'', Dorling Kindersley Inc.: New York (1995) | ||
[[category:geology]] | [[category:geology]] | ||
Revision as of 05:16, January 23, 2008
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)