Albite is the sodium-rich end member of the plagioclase feldspar solid solution series. It is frequently identified by its characteristic polysynthetic twinning visible as striations on crystal faces and its occurrence in igneous pegmatites.
Is this albite?
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 albite with a known reference. Albite 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. Albite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Albite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray, bluish, reddish.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Albite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside albite
Minerals reported to co-occur with albite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- NaAlSi₃O₈
- Mohs hardness
- 6-6.5
- Density
- 2.60-2.63 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Perfect On {001}, Good On {010}
- Rarity
- Common
- Uses
- Collector, Industrial, Ceramic Production
- Host rock
- Granite Pegmatites, Hydrothermal Veins
- Typical price
- $5-50 for small specimens, up to $200 for large display pieces
Where rockhounds find albite
38 mapped spotsClassic worldwide localities
- USA
- Italy
- Brazil
- Norway
- Russia
U.S. states with albite
Each link opens a state-specific list of mapped rockhounding spots that produce albite.
Field-hunting tip
Look in granite pegmatites, hydrothermal veins country — that is the host setting where albite typically forms. If you start seeing quartz, microcline, muscovite 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. In the U.S., the densest reported localities are in Maine, New Jersey, Utah — start trip planning there.





