Gabbro is a dark-colored, coarse-grained intrusive igneous rock composed primarily of plagioclase feldspar and pyroxene. It is the plutonic equivalent of basalt and is often found in large, deep-seated igneous bodies. Collectors frequently seek it for its structural textures and as a source for accessory minerals like magnetite or chromite.
Is this gabbro?
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 gabbro with a known reference. Gabbro sits at Mohs 6-7, softer than the next harder reference, harder than the previous one.
- 2Read the lusterHold the specimen under a strong light. Gabbro typically shows a vitreous luster.
- 3Match the color rangeCompare against the expected color range: black, dark green, dark gray.
- 4Look at form & habitTypical habit: granular.
Often confused with
Gabbro vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside gabbro
Minerals reported to co-occur with gabbro. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Mohs hardness
- 6-7
- Density
- 2.7-3.3 g/cm³
- Colors
- Luster
- Vitreous
- Transparency
- Opaque
- Crystal habit
- Granular
- Cleavage
- None
- Rarity
- Common
- Uses
- Building Stone, Decorative, Industrial
- Host rock
- Plutonic Environments
- Typical price
- $5-30 for slabs or architectural samples
Where rockhounds find gabbro
Classic worldwide localities
- Bushveld Complex, South Africa
- Stillwater Complex, USA
- Duluth Complex, USA
- Skye, Scotland
- Norway
Field-hunting tip
Look in plutonic environments country, the host setting where gabbro typically forms. If you start seeing plagioclase, pyroxene, olivine in float, you are in the right ground. Field specimens usually show a granular habit, so train your eye for that shape before scanning the outcrop.







