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, 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.







