Henrymeyerite is a very rare barium-iron-titanium oxide belonging to the hollandite group. It typically appears as small, black, prismatic to needle-like crystals occurring within alkaline rock complexes. Collectors primarily find this mineral in the Kovdor Massif of Russia, where it is often associated with magnetite and silicate minerals.
Is this henrymeyerite?
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 henrymeyerite with a known reference. Henrymeyerite sits at Mohs 6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Henrymeyerite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Henrymeyerite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: tetragonal. Typical habit: prismatic to acicular crystals.
Often confused with
Henrymeyerite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside henrymeyerite
Minerals reported to co-occur with henrymeyerite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaFe²⁺Ti₇O₁₆
- Mohs hardness
- 6
- Density
- 4.95 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Tetragonal
- Crystal habit
- Prismatic to Acicular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector, Scientific Research
- Host rock
- Alkaline Ultramafic Rocks
- Typical price
- $50-300 per specimen
Where rockhounds find henrymeyerite
Classic worldwide localities
- Kovdor Massif, Kola Peninsula, Russia
Field-hunting tip
Look in alkaline ultramafic rocks country — that is the host setting where henrymeyerite typically forms. If you start seeing magnetite, forsterite, phlogopite in float, you are in the right ground. Field specimens usually show a prismatic to acicular crystals habit, so train your eye for that shape before scanning the outcrop.







