Gypsite is an earthy, incoherent mixture of gypsum and clay or other impurities found in surface deposits. It typically forms as a powdery or crumbly material in arid regions where groundwater evaporates near the surface, leaving behind gypsum-rich crusts.
Is this gypsite?
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 gypsite with a known reference. Gypsite sits at Mohs 1.5-2 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Gypsite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Gypsite typically shows a dull luster.
- 4Match the color rangeCompare against the expected color range: white, gray, yellowish, brownish.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: earthy.
Often found alongside gypsite
Minerals reported to co-occur with gypsite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaSO₄·2H₂O
- Mohs hardness
- 1.5-2
- Density
- 2.3 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Earthy
- Cleavage
- None
- Rarity
- Common
- Uses
- Agricultural, Industrial
- Host rock
- Evaporite Deposits
- Typical price
- $1-10 per specimen
Where rockhounds find gypsite
1 mapped spotsClassic worldwide localities
- United States
- Spain
- Mexico
- Australia
- China
Field-hunting tip
Look in evaporite deposits country — that is the host setting where gypsite typically forms. If you start seeing halite, anhydrite, dolomite in float, you are in the right ground. Field specimens usually show a earthy habit, so train your eye for that shape before scanning the outcrop. In the U.S., the densest reported localities are in Utah — start trip planning there.



