Tilasite is a rare calcium magnesium arsenate fluoride mineral often found in metamorphosed ore deposits. It typically occurs as small, prismatic, yellowish to colorless crystals that can be difficult to distinguish from other similar species without mineralogical testing. It is most famous for its occurrence in the classic mining localities of Långban, Sweden, and the Franklin Mining District in New Jersey.
Is this tilasite?
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 tilasite with a known reference. Tilasite sits at Mohs 5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Tilasite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Tilasite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: yellow, yellowish-brown, colorless, white.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, granular.
Often confused with
Tilasite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside tilasite
Minerals reported to co-occur with tilasite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CaMg(AsO₄)F
- Mohs hardness
- 5
- Density
- 3.75-3.85 g/cm³
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Granular
- Cleavage
- Poor
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Metamorphosed Iron-manganese Deposits
- Typical price
- $50-500 depending on quality and locality
Where rockhounds find tilasite
Classic worldwide localities
- Långban, Sweden
- Franklin, New Jersey, USA
- Pioche, Nevada, USA
Field-hunting tip
Look in metamorphosed iron-manganese deposits country — that is the host setting where tilasite typically forms. If you start seeing haematite, barite, willemite in float, you are in the right ground. Field specimens usually show a prismatic crystals, granular habit, so train your eye for that shape before scanning the outcrop.




