Anorthite is the calcium-rich endmember of the plagioclase feldspar solid solution series. It is typically found in calcium-rich mafic igneous rocks or thermally metamorphosed limestone, often appearing as glassy, colorless to white tabular crystals.
Is this anorthite?
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 anorthite with a known reference. Anorthite sits at Mohs 6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Anorthite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Anorthite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray, yellowish.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Anorthite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside anorthite
Minerals reported to co-occur with anorthite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaAl₂Si₂O₈
- Mohs hardness
- 6
- Density
- 2.74-2.76 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Perfect Basal, Good Prismatic
- Rarity
- Uncommon
- Uses
- Collector, Scientific Research
- Host rock
- Mafic Igneous Rocks, Metamorphic Contact Zones
- Typical price
- $10-100 per specimen
Where rockhounds find anorthite
Classic worldwide localities
- Mount Somma, Italy
- Miyake-jima, Japan
- Franklin, New Jersey, USA
- Bushveld Complex, South Africa
Field-hunting tip
Look in mafic igneous rocks, metamorphic contact zones country — that is the host setting where anorthite typically forms. If you start seeing pyroxene, olivine, magnetite in float, you are in the right ground. Field specimens usually show a tabular crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.







