Oligoclase is a common plagioclase feldspar that represents a solid solution between albite and anorthite. It is frequently found in igneous rocks and can exhibit a unique schiller effect known as aventurescence, especially in the variety called sunstone.
Is this oligoclase?
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 oligoclase with a known reference. Oligoclase 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. Oligoclase leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Oligoclase typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, gray, pale yellow, pale green, reddish.
- 5Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals, massive, granular.
Often confused with
Oligoclase vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside oligoclase
Minerals reported to co-occur with oligoclase. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na,Ca)(Si,Al)₄O₈
- Mohs hardness
- 6-6.5
- Density
- 2.64-2.67 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular Crystals, Massive, Granular
- Cleavage
- Perfect Basal and Pinacoidal
- Rarity
- Common
- Uses
- Collector, Petrological Studies, Lapidary
- Host rock
- Granite, Granodiorite, Syenite, Pegmatites
- Typical price
- $5-30 for small samples, $50+ for quality crystalline specimens
Where rockhounds find oligoclase
Classic worldwide localities
- Norway
- Canada
- USA
- Russia
- India
Field-hunting tip
Look in granite, granodiorite, syenite, pegmatites country — that is the host setting where oligoclase typically forms. If you start seeing quartz, muscovite, biotite 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.







