A nodule is a rounded, irregular mass or concretion formed by mineral precipitation around a central nucleus within sedimentary rock. Collectors prize it for what may be inside: a quartz or chalcedony-lined geode, fossilized material, or an unusual crystalline structure. It commonly weathers out of softer host rock such as chalk beds or shale.
Is this nodule?
3-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Read the textureLook at a fresh break with a hand lens. Texture: Small, irregularly rounded lump that contrasts with the enclosing sediment or rock.
- 2Pick out the mineralsComposition: Commonly calcite, chert, apatite (phosphorite), anhydrite or pyrite. Identify the two or three most abundant grains.
- 3Match the color rangeCompare against the expected color range: gray, brown, black, white.
Often found alongside nodule
Minerals reported to co-occur with nodule. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Rarity
- Common
- Uses
- Collector, Lapidary
- Host rock
- sedimentary strata such as limestone, chalk, or shale
- Texture
- Small, irregularly rounded lump that contrasts with the enclosing sediment or rock
- Composition
- Commonly calcite, chert, apatite (phosphorite), anhydrite or pyrite
Where rockhounds find nodule
10 mapped spotsClassic worldwide localities
- United Kingdom
- United States
- France
- Germany
- Poland
Field-hunting tip
Where it forms: sedimentary strata such as limestone, chalk, or shale. If you start seeing chalcedony, calcite, pyrite in float, you are in the right ground. In the U.S., the densest reported localities are in Arizona, Nevada, Utah. Start trip planning there.






