Niigataite is a strontium-rich member of the clinozoisite-epidote group, uniquely identified by its distinctive pink coloration caused by its composition. It is primarily found as an accessory mineral in high-pressure, low-temperature metamorphic rocks in Japan. Collectors look for its well-formed prismatic crystals embedded in quartz or schist matrices.
Is this niigataite?
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 niigataite with a known reference. Niigataite sits at Mohs 6-7 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Niigataite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Niigataite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: pink, reddish-pink.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, radial aggregates, massive.
Often confused with
Niigataite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside niigataite
Minerals reported to co-occur with niigataite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₂SrAl₃(Si₂O₇)(SiO₄)O(OH)
- Mohs hardness
- 6-7
- Density
- 3.5 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Radial Aggregates, Massive
- Cleavage
- Perfect
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphic Rocks
- Typical price
- $20-150 per specimen depending on size and quality
Where rockhounds find niigataite
Classic worldwide localities
- Niigata Prefecture, Japan
- Kochi Prefecture, Japan
Field-hunting tip
Look in metamorphic rocks country — that is the host setting where niigataite typically forms. If you start seeing quartz, albite, calcite in float, you are in the right ground. Field specimens usually show a prismatic crystals, radial aggregates, massive habit, so train your eye for that shape before scanning the outcrop.







