Snakeskin Agate is characterized by a distinctive, intricate surface pattern resembling reptile scales, caused by dehydration and contraction of the silica gel. It is a form of microcrystalline quartz typically found as nodules or cavity linings in volcanic or sedimentary environments. Collectors value it for its unique texture, which takes a high polish during lapidary work.
Is this snakeskin 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 snakeskin agate with a known reference. Snakeskin 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. Snakeskin Agate leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Snakeskin Agate typically shows a waxy luster.
- 4Match the color rangeCompare against the expected color range: white, gray, tan, yellow, brown.
- 5Look at form & habitCrystal system: trigonal. Typical habit: botryoidal.
Often confused with
Snakeskin Agate vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside snakeskin agate
Minerals reported to co-occur with snakeskin 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
- 2.6-2.65 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 Cavities
- Typical price
- $5-50 for slabs or polished cabochons
Where rockhounds find snakeskin agate
Classic worldwide localities
- Wyoming, USA
- Oregon, USA
- California, USA
Field-hunting tip
Look in sedimentary cavities country — that is the host setting where snakeskin agate typically forms. If you start seeing quartz, calcite, zeolites in float, you are in the right ground. Field specimens usually show a botryoidal habit, so train your eye for that shape before scanning the outcrop.




