Pigeonite is a calcium-poor clinopyroxene that is characteristic of rapidly cooled mafic igneous rocks. It is most easily identified in thin section due to its unique optical properties, though in hand samples, it typically appears as brownish-green to black massive grains within basaltic or diabasic matrices.
Is this pigeonite?
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 pigeonite with a known reference. Pigeonite sits at Mohs 5.5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Pigeonite leaves a white streak.
- 3Read the lusterHold the specimen under a strong light. Pigeonite typically shows a vitreous luster.
- 4Match the color rangeCompare against the expected color range: brown, brownish-green, black.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: prismatic crystals, massive, granular.
Often confused with
Pigeonite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside pigeonite
Minerals reported to co-occur with pigeonite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ca,Mg,Fe)₂(Mg,Fe)Si₂O₆
- Mohs hardness
- 5.5-6
- Density
- 3.3-3.5 g/cm³
- Colors
- Streak
- White
- Luster
- Vitreous
- Transparency
- Translucent
- Crystal system
- Monoclinic
- Crystal habit
- Prismatic Crystals, Massive, Granular
- Cleavage
- Good in 2 Directions At Nearly 90 Degrees
- Rarity
- Common
- Uses
- Collector, Scientific Research
- Host rock
- Mafic Igneous Rocks Such as Basalt, Diabase, And Gabbro
- Typical price
- $5-30 per specimen
Where rockhounds find pigeonite
Classic worldwide localities
- Pigeon Point, Minnesota, USA
- Bushveld Complex, South Africa
- Isle of Skye, Scotland
- Lunar basalt samples
- Dolerite sills globally
Field-hunting tip
Look in mafic igneous rocks such as basalt, diabase, and gabbro country — that is the host setting where pigeonite typically forms. If you start seeing plagioclase, augite, olivine in float, you are in the right ground. Field specimens usually show a prismatic crystals, massive, granular habit, so train your eye for that shape before scanning the outcrop.






