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, 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.




