Slawsonite is a rare strontium-bearing feldspar that is primarily valued by mineral collectors for its strong blue fluorescence under short-wave UV light. It is typically found as small, clear to white tabular crystals embedded in metamorphosed limestone or calcium-rich silicate rocks.
Is this slawsonite?
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 slawsonite with a known reference. Slawsonite sits at Mohs 5.5-6.5, 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: colorless, medium gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: aggregates, radial, tabular.
Often confused with
Slawsonite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside slawsonite
Minerals reported to co-occur with slawsonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- SrAl₂Si₂O₈
- Mohs hardness
- 5.5-6.5
- Density
- 3.05 g/cm³
- Colors
- ColorlessMedium gray
- Streak
- White
- Luster
- Vitreous
- Transparency
- Semitransparent
- Crystal system
- Monoclinic
- Crystal habit
- Aggregates, radial, tabular
- Cleavage
- Good on {001}, fair to good on {100}
- Fluorescence
- Pinkish red purple under SW UV
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In pectolite veinlets in metamorphosed xenoliths (Rendai, Japan); in a xenolith in ultramafic rock (Sarusaka, Japan)
Where rockhounds find slawsonite
Classic worldwide localities
- Wallowa Mountains, Wallowa Co., Oregon, USA
- Kochi Prefecture, from Sarusaka, Kamagi, Japan
- Rendai, Kochi City, Japan
- Miyanotani, Hidaka, Japan
Field-hunting tip
Where it forms: In pectolite veinlets in metamorphosed xenoliths (Rendai, Japan); in a xenolith in ultramafic rock (Sarusaka, Japan). If you start seeing calcite, phlogopite, albite in float, you are in the right ground. Typical habit: aggregates, radial, tabular. Train your eye for that shape before scanning the outcrop.







