Amblygonite is a phosphate mineral commonly found in lithium-rich pegmatites. It is often confused with other minerals like spodumene due to similar habits, but it is typically identified by its perfect cleavage and specific density.
Is this amblygonite?
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 amblygonite with a known reference. Amblygonite sits at Mohs 5.5-6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Amblygonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Amblygonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellow, pale blue, greenish, beige.
- 5Look at form & habitCrystal system: triclinic. Typical habit: massive, granular, or rarely as short prismatic crystals.
Often confused with
Amblygonite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside amblygonite
Minerals reported to co-occur with amblygonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Li,Na)AlPO₄(F,OH)
- Mohs hardness
- 5.5-6
- Density
- 3.0-3.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Triclinic
- Crystal habit
- Massive, Granular, Or Rarely as Short Prismatic Crystals
- Cleavage
- Perfect Basal, Good Prismatic
- Fluorescence
- Often Fluorescent White or Yellow Under SW UV
- Rarity
- Uncommon
- Uses
- Collector, Gemstone, Lithium Ore
- Host rock
- Granite Pegmatites
- Typical price
- $10-50 per gram for gem rough, $20-200 for mineral specimens
Where rockhounds find amblygonite
Classic worldwide localities
- Brazil
- USA (California, Maine)
- Namibia
- France
- Germany
Field-hunting tip
Look in granite pegmatites country, the host setting where amblygonite typically forms. If you start seeing spodumene, lepidolite, tourmaline in float, you are in the right ground. Field specimens usually show a massive, granular, or rarely as short prismatic crystals habit, so train your eye for that shape before scanning the outcrop.







