Loseyite is a very rare carbonate mineral almost exclusively found in the Franklin mining district of New Jersey. It is characterized by its delicate, bladed white to light blue crystals that often form radiating clusters on a matrix of other zinc-rich minerals.
Is this loseyite?
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 loseyite with a known reference. Loseyite sits at Mohs ~3, 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.
- 4Match the color rangeCompare against the expected color range: bluish white, brownish, brownish white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: bladed crystals, radial aggregates.
Often confused with
Loseyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside loseyite
Minerals reported to co-occur with loseyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Mn,Zn)₇(CO₃)₂(OH)₁₀
- Mohs hardness
- ~3
- Density
- 3.27 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Bladed crystals, radial aggregates
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- A very rare mineral occurring in veinlets in massive ore in a metamorphosed stratiform zinc orebody
Where rockhounds find loseyite
Classic worldwide localities
- Franklin, Sussex Co., New Jersey, USA
Field-hunting tip
Where it forms: A very rare mineral occurring in veinlets in massive ore in a metamorphosed stratiform zinc orebody. If you start seeing pyrochroite, sussexite, chlorophoenicite in float, you are in the right ground. Typical habit: bladed crystals, radial aggregates. Train your eye for that shape before scanning the outcrop.





