Mimetite is a striking lead arsenate mineral often found in the oxidized zones of base metal deposits. Collectors value it for its vivid yellow-to-orange hues and its aesthetic botryoidal or hexagonal crystal habits, frequently appearing alongside wulfenite.
Is this mimetite?
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 mimetite with a known reference. Mimetite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Mimetite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Mimetite typically shows a adamantine luster.
- 4Match the color rangeCompare against the expected color range: yellow, orange, brown, colorless, white.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: prismatic crystals, botryoidal, crusts, globular.
Often confused with
Mimetite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside mimetite
Minerals reported to co-occur with mimetite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Pb₅(AsO₄)₃Cl
- Mohs hardness
- 3.5-4
- Density
- 7.1-7.3 g/cm³
- Streak
- White
- Luster
- Adamantine
- Transparency
- Translucent
- Crystal system
- Hexagonal
- Crystal habit
- Prismatic Crystals, Botryoidal, Crusts, Globular
- Cleavage
- Poor
- Rarity
- Uncommon
- Uses
- Collector
- Host rock
- Oxidized Zones of Lead-arsenic Mineral Deposits
- Typical price
- $20-200 depending on crystal size and location
Where rockhounds find mimetite
Classic worldwide localities
- Johanngeorgenstadt, Germany
- Mapimi, Mexico
- Tsumeb, Namibia
- Broken Hill, Australia
Field-hunting tip
Look in oxidized zones of lead-arsenic mineral deposits country — that is the host setting where mimetite typically forms. If you start seeing galena, cerussite, wulfenite in float, you are in the right ground. Field specimens usually show a prismatic crystals, botryoidal, crusts, globular habit, so train your eye for that shape before scanning the outcrop.






