A chalcedony nodule typically forms as a rounded, botryoidal mass within a rock cavity or as a sedimentary concretion. It is recognized by its waxy luster, the absence of crystalline structure visible to the naked eye, and its characteristically smooth, mammillary surface.
Is this chalcedony nodule?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch chalcedony nodule with a known reference. Chalcedony Nodule sits at Mohs 6.5-7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: waxy.
- 4Match the color rangeCompare against the expected color range: white, gray, blue, brown, tan.
- 5Look at form & habitCrystal system: trigonal. Typical habit: botryoidal.
Often confused with
Chalcedony Nodule vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Luster reads waxy on Chalcedony Nodule and vitreous to dull on Opal.

How to tell apart: Chalcedony Nodule is noticeably harder (Mohs 6.5-7 vs. 4-4.5); luster reads waxy on Chalcedony Nodule and vitreous, may be pearly on Smithsonite.

How to tell apart: Luster reads waxy on Chalcedony Nodule and vitreous, weak pearly on {001} on Prehnite.
Often found alongside chalcedony nodule
Minerals reported to co-occur with chalcedony nodule. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SiO₂
- Mohs hardness
- 6.5-7
- Density
- 2.6-2.65 g/cm³
- Streak
- White
- Luster
- Waxy
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Botryoidal
- Cleavage
- None
- Rarity
- Common
- Uses
- Lapidary, Collector, Decorative
- Host rock
- sedimentary and volcanic cavities
Where rockhounds find chalcedony nodule
2 mapped spotsClassic worldwide localities
- USA
- Mexico
- Brazil
- India
- Madagascar
Field-hunting tip
Where it forms: sedimentary and volcanic cavities. If you start seeing quartz, calcite, goethite in float, you are in the right ground. Typical habit: botryoidal. Train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Tennessee, Washington. Start trip planning there.





