Prairie Agate is a variety of chalcedony typically found as nodules in the Great Plains region of the United States. It is prized by lapidary artists for its warm, earthy tones and unique banding patterns, which often resemble desert landscapes or complex swirling fortifications.
Is this prairie 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 prairie agate with a known reference. Prairie 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. Prairie Agate leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Prairie Agate typically shows a waxy luster.
- 4Match the color rangeCompare against the expected color range: yellow, brown, orange, cream, white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: nodular.
Often confused with
Prairie Agate vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside prairie agate
Minerals reported to co-occur with prairie 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
- 2.6-2.7 g/cm³
- Streak
- White
- Luster
- Waxy
- Transparency
- Translucent
- Crystal system
- Trigonal
- Crystal habit
- Nodular
- Cleavage
- None
- Rarity
- Common
- Uses
- Lapidary, Collector, Decorative
- Host rock
- Sedimentary
- Typical price
- $5-50 for slabs and cabochons
Where rockhounds find prairie agate
Classic worldwide localities
- Wyoming, USA
- Nebraska, USA
- South Dakota, USA
Field-hunting tip
Look in sedimentary country — that is the host setting where prairie agate typically forms. If you start seeing calcite, quartz, chalcedony in float, you are in the right ground. Field specimens usually show a nodular habit, so train your eye for that shape before scanning the outcrop.





