Vonsenite is a rare iron-rich borate mineral typically found as black, acicular, or prismatic crystals within contact metamorphic zones. It is often distinguished from similar iron minerals by its occurrence in specific boron-bearing skarns and its submetallic luster.
Is this vonsenite?
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 vonsenite with a known reference. Vonsenite 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. Vonsenite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Vonsenite typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: orthorhombic. Typical habit: acicular or prismatic crystals, commonly in radiating aggregates or massive forms.
Often confused with
Vonsenite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside vonsenite
Minerals reported to co-occur with vonsenite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₂²⁺Fe³⁺BO₅
- Mohs hardness
- 5
- Density
- 4.5-4.8 g/cm³
- Colors
- Streak
- Black
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Acicular or Prismatic Crystals, Commonly in Radiating Aggregates or Massive Forms
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Research
- Host rock
- Contact Metamorphic Zones in Limestone
- Typical price
- $20-150 for thumbnail to small cabinet specimens
Where rockhounds find vonsenite
Classic worldwide localities
- Riverside County, California, USA
- Brooks Mountain, Alaska, USA
- Dognecea, Romania
- Sayama, Japan
Field-hunting tip
Look in contact metamorphic zones in limestone country, the host setting where vonsenite typically forms. If you start seeing calcite, magnetite, forsterite in float, you are in the right ground. Field specimens usually show a acicular or prismatic crystals, commonly in radiating aggregates or massive forms habit, so train your eye for that shape before scanning the outcrop.






