Minrecordite is a rare zinc-dominant member of the dolomite group, often found as small, sharp rhombohedral crystals in the oxidized zones of metal mines. It is visually indistinguishable from dolomite to the naked eye, requiring chemical analysis for positive identification. It is most famously collected from the Tsumeb Mine in Namibia, where it occurs alongside other rare zinc secondary minerals.
Is this minrecordite?
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 minrecordite with a known reference. Minrecordite sits at Mohs 3.5, 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: vitreous to pearly.
- 4Match the color rangeCompare against the expected color range: colorless, white.
- 5Look at form & habitCrystal system: trigonal. Typical habit: rhombohedral crystals.
Often confused with
Minrecordite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside minrecordite
Minerals reported to co-occur with minrecordite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaZn(CO₃)₂
- Mohs hardness
- 3.5
- Density
- 3.45 g/cm³
- Streak
- White
- Luster
- Vitreous to pearly
- Transparency
- Semitransparent
- Crystal system
- Trigonal
- Crystal habit
- Rhombohedral crystals
- Cleavage
- On {1014}, prominent
- Rarity
- Rare
- Uses
- Collector, Scientific research
- Host rock
- In a dolostone-hosted hydrothermal polymetallic ore deposit (Tsumeb, Namibia); from the wallrock of a carbonate-hosted Pb–Zn orebody (Navan deposit, Ireland)
Where rockhounds find minrecordite
Classic worldwide localities
- Centennial Eureka mine, Tintic district, Juab Co., Utah, USA
- Tsumeb, Namibia
- Navan Pb–Zn orebody, Co. Meath, Ireland
Field-hunting tip
Where it forms: In a dolostone-hosted hydrothermal polymetallic ore deposit (Tsumeb, Namibia); from the wallrock of a carbonate-hosted Pb–Zn orebody (Navan deposit, Ireland). If you start seeing dioptase, duftite, malachite in float, you are in the right ground. Typical habit: rhombohedral crystals. Train your eye for that shape before scanning the outcrop.








