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Sill identification and geology
A tabular body of intrusive igneous rock that is concordant—parallel to the bedding or foliation of the surrounding country rock. Sills form when magma is injected along pre-existing planes of weakness bedding planes, foliation surfaces and crystallizes in place. They range from centimeters to hundreds of meters in thickness and can extend for many kilometers laterally. Field: petrology. Example: The Whin Sill of northern England is a dolerite diabase sill up to 70 m thick that was intruded into Carboniferous sedimentary rocks approximately 295 million years ago and forms the foundation of parts of Hadrian's Wall.. Related terms: Dike, Concordant, Intrusion, Laccolith.
Sources, scope & corrections
These authoritative resources support category-level nomenclature, terminology, identification methods, and safety. When a specimen-specific safety warning appears, the public-health source listed here directly supports that precaution. They are not line-by-line citations for every other property on this entry, and natural specimens vary.
- Editorial owner
- GeoMiner
- Last updated
- 2026-03-30T15:19:42.096023+00:00
- Review status
- Published; not independently peer-reviewed
- USGS Thesaurus — U.S. Geological Survey. Controlled earth-science terminology used to describe USGS information resources.
- Glossary of Geologic Terms — U.S. National Park Service. Geologic definitions prepared by the NPS Geologic Resources Inventory.
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