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, 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.







