Ardennite-(V) is a rare manganese-vanadium sorosilicate mineral that typically forms as prismatic to acicular crystals within manganese deposits. It is most recognized for its distinct yellow-brown color and its association with other manganese-rich silicate minerals in metamorphosed sedimentary environments.
Is this ardennite-(v)?
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 ardennite-(v) with a known reference. Ardennite-(V) sits at Mohs 6-7, 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: vitreous.
- 4Match the color rangeCompare against the expected color range: yellow.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular, tabular.
Often confused with
Ardennite-(V) vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside ardennite-(v)
Minerals reported to co-occur with ardennite-(v). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Mn₄(AlMg)Al₄(Si₅V)O₂₂(OH)₆
- Mohs hardness
- 6-7
- Density
- 3.55 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Transparent
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular, tabular
- Cleavage
- None observed
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In a quartz veinlet in piemontite-bearing mica schist
Where rockhounds find ardennite-(v)
Classic worldwide localities
- Sparone, Locana Valley (TO), Piedmont, Italy
Field-hunting tip
Where it forms: In a quartz veinlet in piemontite-bearing mica schist. If you start seeing quartz, piemontite, hematite in float, you are in the right ground. Typical habit: acicular, tabular. Train your eye for that shape before scanning the outcrop.






