Sauconite is a zinc-rich member of the smectite clay group, typically forming as a secondary mineral in the oxidation zones of zinc deposits. It is rarely found in distinct crystals and usually appears as massive, earthy, or waxy coatings and aggregates, making it primarily a specimen for specialized mineral collectors.
Is this sauconite?
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 sauconite with a known reference. Sauconite sits at Mohs 1-2, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: dull.
- 4Match the color rangeCompare against the expected color range: bluish white, reddish brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: earthy, massive.
Often confused with
Sauconite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside sauconite
Minerals reported to co-occur with sauconite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Na₀.₃Zn₃(Si₃Al)O₁₀(OH)₂·4H₂O
- Mohs hardness
- 1-2
- Density
- 2.45 g/cm³
- Streak
- White
- Luster
- Dull
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Earthy, massive
- Cleavage
- {001}, perfect
- Rarity
- Rare
- Uses
- Collector, Mineralogical study
- Host rock
- Fills vugs and seams in oxidized zinc and copper deposits; may be redeposited at the water table
Where rockhounds find sauconite
Classic worldwide localities
- Ueberroth mine, Saucon Valley, near Friedensville, Lehigh Co., Pennsylvania, USA
- Coon Hollow mine, north of Zinc, Boone Co., Arkansas, USA
- Liberty mine, Meekers Grove, Lafayette Co., Wisconsin, USA
- Castle Dome, Globe-Miami district, and the 79 mine, Gila Co., and from the Magma mine, Superior, Pinal Co., Arizona, USA
Field-hunting tip
Where it forms: Fills vugs and seams in oxidized zinc and copper deposits; may be redeposited at the water table. If you start seeing hemimorphite, smithsonite, chrysocolla in float, you are in the right ground. Typical habit: earthy, massive. Train your eye for that shape before scanning the outcrop.







