Montebrasite is a lithium-rich phosphate mineral occurring primarily in granitic pegmatites. It is often found as massive, cleavable blocks and is visually indistinguishable from amblygonite without chemical analysis, as they form a continuous solid solution series.
Is this montebrasite?
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 montebrasite with a known reference. Montebrasite 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. Montebrasite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Montebrasite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: white, colorless, yellow, greenish, gray.
- 5Look at form & habitCrystal system: triclinic. Typical habit: massive, thick tabular crystals.
Often confused with
Montebrasite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside montebrasite
Minerals reported to co-occur with montebrasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- LiAlPO₄(OH)
- Mohs hardness
- 5.5-6
- Density
- 3.0-3.1 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Massive, Thick Tabular Crystals
- Cleavage
- Perfect Basal
- Rarity
- Uncommon
- Uses
- Collector, Lithium Source
- Host rock
- Granite Pegmatites
- Typical price
- $10-100 per specimen
Where rockhounds find montebrasite
Classic worldwide localities
- Montebras, France
- Minas Gerais, Brazil
- Newry, Maine, USA
- Black Hills, South Dakota, USA
- Karibib, Namibia
Field-hunting tip
Look in granite pegmatites country — that is the host setting where montebrasite typically forms. If you start seeing lepidolite, tourmaline, cassiterite in float, you are in the right ground. Field specimens usually show a massive, thick tabular crystals habit, so train your eye for that shape before scanning the outcrop.







