Spadaite is a rare, hydrated magnesium silicate that typically appears in massive, waxy, or compact forms. It is most commonly found in cavities within igneous rocks or associated with serpentine and hydrothermal deposits.
Is this spadaite?
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 spadaite with a known reference. Spadaite sits at Mohs 2.5, 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: pearly or greasy.
- 4Match the color rangeCompare against the expected color range: colorless, cream, pinkish.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: amorphous, massive.
Often confused with
Spadaite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside spadaite
Minerals reported to co-occur with spadaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- MgSiO₃·nH₂O
- Mohs hardness
- 2.5
- Density
- 2.2 g/cm³
- Streak
- White
- Luster
- Pearly or greasy
- Transparency
- Translucent
- Crystal system
- Orthorhombic
- Crystal habit
- Amorphous, massive
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In leucite-bearing lava (Capo di Bove, Italy); in amygdular diabase (Sasbach, Germany); replacing tactite minerals near gold ore shoots (Gold Hill, Utah, USA)
Where rockhounds find spadaite
Classic worldwide localities
- Cane Springs, Alvarado, and Midas mines, near Gold Hill, Tooele Co., Utah, and in the Livingston quarry, Palos Verdes Hills, Los Angeles Co., California, USA
- Capo di Bove, near Rome, Lazio, Italy
- Sasbach, Baden-Württemberg, Germany
Field-hunting tip
Where it forms: In leucite-bearing lava (Capo di Bove, Italy); in amygdular diabase (Sasbach, Germany); replacing tactite minerals near gold ore shoots (Gold Hill, Utah, USA). If you start seeing wollastonite, diopside, garnet in float, you are in the right ground. Typical habit: amorphous, massive. Train your eye for that shape before scanning the outcrop.





