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 6-6.5, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray, yellowish, gray, red, reddish gray.
- 5Look at form & habitCrystal system: triclinic. Typical habit: euhedral crystals, granular, striated.
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
- 6-6.5
- Density
- 2.74-2.76 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Crystal system
- Triclinic
- Crystal habit
- Euhedral crystals, granular, striated
- Cleavage
- Perfect on {001}, less so on {010}, imperfect on {110}
- Rarity
- Uncommon
- Uses
- Collector, Scientific research
- Host rock
- A rare constituent of mafic plutonic and volcanic rocks
Where rockhounds find anorthite
Classic worldwide localities
- Great Sitkin Island, Aleutian Islands, Alaska, USA
- Grass Valley, Nevada Co., California, USA
- Monte Somma and Vesuvius, Campania, Italy
- Mt. Monzoni, Val di Fassa, Trentino-Alto Adige, Italy
- Cyclopean Islands, Italy
- Tunaberg, Södermanland, Sweden
Field-hunting tip
Where it forms: A rare constituent of mafic plutonic and volcanic rocks. If you start seeing olivine, pyroxene, corundum in float, you are in the right ground. Typical habit: euhedral crystals, granular, striated. Train your eye for that shape before scanning the outcrop.






