Suseinargiuite is a rare sodium bismuth molybdate that forms colorless acicular crystals in hemispherical aggregates. It formed by hydrothermal and/or supergene alteration of a primary Mo-Bi mineral assemblage. Associated minerals include wulfenite, molybdenite and chalcopyrite. It was first described from Su Seinargiu, northwest of Sarroch, Cagliari, Sardinia, Italy.
Is this suseinargiuite?
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 suseinargiuite with a known reference. Suseinargiuite sits at Mohs 2-3, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: pearly to adamantine.
- 3Match the color rangeCompare against the expected color range: colorless.
- 4Look at form & habitCrystal system: tetragonal. Typical habit: acicular crystals form hemispherical aggregates.
Often confused with
Suseinargiuite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside suseinargiuite
Minerals reported to co-occur with suseinargiuite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Na₀.₅Bi₀.₅)(MoO₄)
- Mohs hardness
- 2-3
- Density
- 5.597 g/cm³
- Colors
- Luster
- Pearly to adamantine
- Transparency
- Transparent
- Crystal system
- Tetragonal
- Crystal habit
- Acicular crystals form hemispherical aggregates
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed by hydrothermal and/or supergene alteration of a primary Mo-Bi mineral assemblage
Where rockhounds find suseinargiuite
Classic worldwide localities
- Su Seinargiu, northwest of Sarroch, Cagliari, Sardinia, Italy
Field-hunting tip
Where it forms: Formed by hydrothermal and/or supergene alteration of a primary Mo-Bi mineral assemblage. If you start seeing wulfenite, molybdenite, chalcopyrite in float, you are in the right ground. Typical habit: acicular crystals form hemispherical aggregates. Train your eye for that shape before scanning the outcrop.








