An oolitic agate is a distinctive chalcedony specimen featuring small, spherical ooids formed by concentric layers of silica around a nucleus. It occurs in sedimentary environments, showing a textured, bead-like surface that often reveals complex patterning when polished for lapidary use.
Is this oolitic agate?
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 oolitic agate with a known reference. Oolitic Agate 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, brown, tan, red.
- 5Look at form & habitCrystal system: trigonal. Typical habit: botryoidal.
Often confused with
Oolitic Agate vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside oolitic agate
Minerals reported to co-occur with oolitic agate. 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
- 2.65 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
Where rockhounds find oolitic agate
2 mapped spotsClassic worldwide localities
- Wyoming
- Utah
- Montana
- Nevada
Field-hunting tip
Where it forms: sedimentary. If you start seeing calcite, dolomite, quartz 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 Iowa, Oregon. Start trip planning there.






