Difference between revisions of "Sill"
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A '''sill''' is a [[concordant]], sheet-shaped [[Igneous Rock|igneous]] [[intrusion]]. | A '''sill''' is a [[concordant]], sheet-shaped [[Igneous Rock|igneous]] [[intrusion]]. | ||
| − | Pellant, p. 251 | + | Pellant, p. 251 |
==Sources== | ==Sources== | ||
Latest revision as of 19:19, July 13, 2016
A sill is a concordant, sheet-shaped igneous intrusion.
Pellant, p. 251
Sources
- Pellant, Chris. The Complete Book of Rocks and Minerals, Dorling Kindersley Inc.: New York (1995)