Difference between revisions of "Graded Bedding"
Jump to navigation
Jump to search
(Replaced content with 'WOW, THANKS CP! HOW INSIGHTFUL!') |
|||
| 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.<ref>Pellant, p. 250</ref> | |
| + | ==Notes== | ||
| + | {{reflist}} | ||
| + | ==References== | ||
| + | *Pellant, Chris. ''The Complete Book of Rocks and Minerals'', Dorling Kindersley Inc.: New York (1995) | ||
| + | |||
| + | [[category:geology]] | ||
Revision as of 18:13, June 21, 2010
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)