Haggertyite is an extremely rare barium-iron-titanium oxide mineral typically found in metamorphic sanbornite deposits. Collectors should look for distinct, small black tabular crystals associated with barium minerals in California localities.
Is this haggertyite?
4-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 haggertyite with a known reference. Haggertyite sits at Mohs 5, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: metallic.
- 3Match the color rangeCompare against the expected color range: gray.
- 4Look at form & habitCrystal system: hexagonal. Typical habit: tabular crystals.
Often confused with
Haggertyite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside haggertyite
Minerals reported to co-occur with haggertyite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- BaMgFe₄Fe₂Ti₅O₁₉
- Mohs hardness
- 5
- Density
- 4.74 g/cm³
- Colors
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- As isolated crystals or in small groups within the reaction rims around serpentinized mafic xenoliths in olivine lamproite (Arkansas); in the groundmass of diamondiferous olivine lamproite pipes (Australia)
Where rockhounds find haggertyite
Classic worldwide localities
- Prairie Creek lamproite, Crater of Diamonds State Park, near Murfreesboro, Pike County, Arkansas, USA
- Walgidee Hills and the Ellendale 9 pipe, West Kimberley region, Western Australia
Field-hunting tip
Where it forms: As isolated crystals or in small groups within the reaction rims around serpentinized mafic xenoliths in olivine lamproite (Arkansas); in the groundmass of diamondiferous olivine lamproite pipes (Australia). If you start seeing ti-k richterite, diopside, chrome-spinel in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.







