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Syncline identification and geology
A fold in layered rock in which the strata dip inward toward the fold axis from both sides, forming a trough-like shape. In a syncline that has not been overturned, the youngest rocks are found in the core. Synclines and anticlines typically occur together as complementary fold pairs in regions of compressional deformation. Field: structural geology. Example: The Nittany Valley in central Pennsylvania occupies a broad syncline in Paleozoic sedimentary rocks, with resistant sandstone forming ridges on the fold limbs and softer limestone and shale eroded into the valley floor.. Related terms: Anticline, Fold, Trough, Compression.
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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