Metavariscite is a dimorph of variscite that typically occurs in phosphate-rich hydrothermal veins. Collectors usually identify it by its specific tabular crystal habit and distinct green color when found in association with other aluminum phosphates.
Is this metavariscite?
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 metavariscite with a known reference. Metavariscite 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. Metavariscite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Metavariscite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: green, yellow-green.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals, crusts, massive.
Often confused with
Metavariscite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside metavariscite
Minerals reported to co-occur with metavariscite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- AlPO₄·2H₂O
- Mohs hardness
- 3.5-4
- Density
- 2.5 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals, Crusts, Massive
- Cleavage
- Perfect in One Direction
- Rarity
- Rare
- Uses
- Collector, Mineral Specimen
- Host rock
- Phosphate-rich Hydrothermal Deposits
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find metavariscite
Classic worldwide localities
- Little Green Monster Mine, Utah, USA
- Montebras, France
- Cerro de los এখানকার, Spain
- Odenwald, Germany
Field-hunting tip
Look in phosphate-rich hydrothermal deposits country — that is the host setting where metavariscite typically forms. If you start seeing variscite, wardite, crandallite in float, you are in the right ground. Field specimens usually show a tabular crystals, crusts, massive habit, so train your eye for that shape before scanning the outcrop.





