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, 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.







