Zincohögbomite-2N2S is a rare complex oxide mineral belonging to the högbomite group, characterized by a high zinc content. It is typically found in high-grade metamorphic rocks as small, dark, tabular crystals that can be difficult to distinguish from spinel without chemical analysis.
Is this zincohögbomite-2n2s?
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 zincohögbomite-2n2s with a known reference. Zincohögbomite-2N2S sits at Mohs 7, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: brownish.
- 3Read the lusterHold the specimen under a strong light. Luster: adamantine.
- 4Match the color rangeCompare against the expected color range: deep brown, black.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: euhedral crystals, pseudo tetragonal.
Often confused with
Zincohögbomite-2N2S vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside zincohögbomite-2n2s
Minerals reported to co-occur with zincohögbomite-2n2s. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Zn,Al,Fe)₃(Al,Fe,Ti)₈O₁₅(OH)
- Mohs hardness
- 7
- Density
- 4.36 g/cm³
- Colors
- Deep brownBlack
- Streak
- Brownish
- Luster
- Adamantine
- Transparency
- Transparent
- Crystal system
- Hexagonal
- Crystal habit
- Euhedral crystals, pseudo tetragonal
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed by breakdown of gahnite in diasporites (diaspore-bearing metabauxites) and emeries (corundum-bearing metabauxites)
Where rockhounds find zincohögbomite-2n2s
Classic worldwide localities
- Emory deposit at Kerketefs Mountain, Samos Island, Greece (type locality)
Field-hunting tip
Where it forms: Formed by breakdown of gahnite in diasporites (diaspore-bearing metabauxites) and emeries (corundum-bearing metabauxites). If you start seeing spinel, magnetite, corundum in float, you are in the right ground. Typical habit: euhedral crystals, pseudo tetragonal. Train your eye for that shape before scanning the outcrop.




