Scholzite is a rare phosphate mineral often forming delicate, needle-like or prismatic crystal sprays. It is most frequently found in phosphate-rich zones of pegmatites or secondary deposits, appearing as transparent to white crusts or distinct, elongated crystals.
Is this scholzite?
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 scholzite with a known reference. Scholzite sits at Mohs 3-4, 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: colorless, gray white, white.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic crystals, spray-like aggregates.
Often confused with
Scholzite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside scholzite
Minerals reported to co-occur with scholzite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaZn₂(PO₄)₂·2H₂O
- Mohs hardness
- 3-4
- Density
- 3.11-3.13 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic crystals, spray-like aggregates
- Cleavage
- On {100}, fair, a parting with parascholzite lamellae
- Rarity
- Rare
- Uses
- Collector
- Host rock
- May be a primary mineral, but more commonly a secondary mineral in Zn phosphate-bearing granite pegmatites and sediments
Where rockhounds find scholzite
Classic worldwide localities
- Tip Top mine, 8.5 km southwest of Custer, Custer Co., South Dakota, USA
- Snowstorm mine, North Battle Mountain district, Lander Co., Nevada, USA
- Hagendorf, Bavaria, Germany
- Otov, near Domažlice, Czech Republic
- Baccu Locci mine, Cagliari, Sardinia, Italy
- Richelle, near Visé, Belgium
Field-hunting tip
Where it forms: May be a primary mineral, but more commonly a secondary mineral in Zn phosphate-bearing granite pegmatites and sediments. If you start seeing parascholzite, sphalerite, triplite in float, you are in the right ground. Typical habit: prismatic crystals, spray-like aggregates. Train your eye for that shape before scanning the outcrop.







