Khesinite is an extremely rare calcium-iron oxide mineral discovered in xenoliths within volcanic rocks. It typically occurs as small, black, tabular crystals and is scientifically significant due to its unique chemical structure related to the melilite group.
Is this khesinite?
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 khesinite with a known reference. Khesinite sits at Mohs 6, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Luster: semi-metallic.
- 3Match the color rangeCompare against the expected color range: black, dark brown on thin edges.
- 4Look at form & habitCrystal system: triclinic. Typical habit: tabular crystals.
Often confused with
Khesinite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside khesinite
Minerals reported to co-occur with khesinite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Ca₄(Mg₂Fe³⁺₁₀)O₄(Fe³⁺₁₀Si₂)O₃₆
- Mohs hardness
- 6
- Density
- 4.097 g/cm³
- Colors
- BlackDark brown on thin edges
- Luster
- Semi-metallic
- Transparency
- Translucent
- Crystal system
- Triclinic
- Crystal habit
- Tabular crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Formed from melt and as reaction rims in thin veins of paralava within fine-grained gehlenite rocks (pyrometamorphic hornfels)
Where rockhounds find khesinite
Classic worldwide localities
- Gurim anticline, near Arad city, Negev Desert, Israel
Field-hunting tip
Where it forms: Formed from melt and as reaction rims in thin veins of paralava within fine-grained gehlenite rocks (pyrometamorphic hornfels). If you start seeing gehlenite, rankinite, schorlomite in float, you are in the right ground. Typical habit: tabular crystals. Train your eye for that shape before scanning the outcrop.






