Rainbow Moonstone is technically a variety of Labradorite feldspar that exhibits a characteristic adularescence, or schiller, displaying flashes of blue and multi-colored light. It is commonly found in India and Sri Lanka, often fashioned into cabochons to best display its optical play-of-color. Collectors should look for high translucency and strong blue spectral flashes when evaluating specimens.
Is this rainbow moonstone?
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 rainbow moonstone with a known reference. Rainbow Moonstone sits at Mohs 6-6.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Rainbow Moonstone leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Rainbow Moonstone typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, blue, rainbow.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Rainbow Moonstone vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside rainbow moonstone
Minerals reported to co-occur with rainbow moonstone. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- KAlSi₃O₈
- Mohs hardness
- 6-6.5
- Density
- 2.56-2.63 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- Perfect in Two Directions
- Rarity
- Common
- Uses
- Gemstone, Lapidary, Collector
- Host rock
- Pegmatites
- Typical price
- $10-100 per carat for gem-grade material
Where rockhounds find rainbow moonstone
Classic worldwide localities
- India
- Sri Lanka
- Madagascar
- Australia
Field-hunting tip
Look in pegmatites country, the host setting where rainbow moonstone typically forms. If you start seeing quartz, muscovite, biotite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.







