Cassagnaite is an extremely rare calcium vanadium silicate mineral typically found as small, vibrant reddish-golden brown tabular crystals. It is currently known primarily from its type locality in the Cassagna mine of Italy, where it occurs within manganese-rich metamorphic deposits.
Is this cassagnaite?
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 cassagnaite with a known reference. Cassagnaite sits at Mohs 4, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: nearly white.
- 3Read the lusterHold the specimen under a strong light. Luster: vitreous.
- 4Match the color rangeCompare against the expected color range: golden brown.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: prismatic, tabular.
Often confused with
Cassagnaite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Vesuvianite is the harder of the two (Mohs 6-7 vs. 4); streak differs, so Cassagnaite leaves nearly white, Vesuvianite leaves white.

How to tell apart: Garnet is the harder of the two (Mohs 6.5-7.5 vs. 4); streak differs, so Cassagnaite leaves nearly white, Garnet leaves white.
Often found alongside cassagnaite
Minerals reported to co-occur with cassagnaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄Fe₄V₂(OH)₆O₂(Si₃O₁₀)(SiO₄)₂
- Mohs hardness
- 4
- Density
- 3.22 g/cm³
- Colors
- Streak
- Nearly white
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Prismatic, tabular
- Cleavage
- {001} (or parting)
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Filling fractures in braunite and quartz layered mineralization developed under prehnite-pumpellyite facies metamorphism
Where rockhounds find cassagnaite
Classic worldwide localities
- Cassagna mine, Graveglia manganese district, Northern Apennines, Liguria, Italy
Field-hunting tip
Where it forms: Filling fractures in braunite and quartz layered mineralization developed under prehnite-pumpellyite facies metamorphism. If you start seeing braunite, quartz, piemontite in float, you are in the right ground. Typical habit: prismatic, tabular. Train your eye for that shape before scanning the outcrop.



