Mammothite is a rare lead-copper sulfate-carbonate mineral typically found as small, thin, platy crystals. It is a secondary mineral primarily sourced from the historic oxidized zones of lead-copper mines like those in Tiger, Arizona. Collectors prize it for its rarity and its association with other colorful secondary lead minerals.
Is this mammothite?
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 mammothite with a known reference. Mammothite sits at Mohs 2.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Mammothite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Mammothite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, pale yellow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: platy crystals, crusts.
Often confused with
Mammothite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside mammothite
Minerals reported to co-occur with mammothite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₆Cu₄(SO₄)₂(OH)₁₂(CO₃)
- Mohs hardness
- 2.5
- Density
- 4.9-5.0 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Platy Crystals, Crusts
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Oxidized Lead-copper Ore Deposits
- Typical price
- $50-300 per specimen
Where rockhounds find mammothite
Classic worldwide localities
- Mammoth-St. Anthony mine, Arizona, USA
- Tiger, Arizona, USA
Field-hunting tip
Look in oxidized lead-copper ore deposits country — that is the host setting where mammothite typically forms. If you start seeing cerussite, anglesite, diaboleite in float, you are in the right ground. Field specimens usually show a platy crystals, crusts habit, so train your eye for that shape before scanning the outcrop.




