Gabbro specimen

Crystal & mineral guide

Gabbro

Mafic intrusive rock

IgneousRock

Coarse mafic intrusive equivalent of basalt — dense dark rock.

Identify Gabbro with RockScan

About Gabbro

Gabbro is the plutonic cousin of basalt: coarse dark interlocking plagioclase and pyroxene. Forms significant parts of oceanic crust and layered intrusions that may host chromite/PGE ores. Heavier and darker than granite.

Gabbro belongs in a crystal identifier workflow because photo cues — color zoning, crystal habit, and surface luster — combine with measurable traits like Mohs 5–6 (aggregate) and specific gravity 2.9–3.2. Use RockScan’s camera to get a first-pass ID, then confirm with the checklist below.

Gabbro properties

Mohs hardness5–6 (aggregate)
Crystal systemPhaneritic aggregate
LusterVitreous to dull
ColorDark gray to black-green
CompositionPlagioclase + pyroxene ± olivine (basalt chemistry)
FormationSlow cooling of mafic magma at depth
OccurrenceLayered intrusions, ophiolites, oceanic crust Layer 3
Specific gravity2.9–3.2
CleavageNone

How to identify Gabbro

  1. Coarse dark rock without quartz
  2. Dense feel
  3. Green-black pyroxene + pale plagioclase

Collector notes

  • Oceanic Layer 3 is largely gabbroic
  • Some ornamental 'black granite' is actually gabbro

Value context: Dimension stone and aggregate; ore-hosting gabbros valued for mineralization.

Gabbro FAQ

How do you identify Gabbro?

Gabbro (Mafic intrusive rock) is typically recognized by dark gray to black-green color, vitreous to dull luster, Mohs hardness 5–6 (aggregate), and phaneritic aggregate crystal system. RockScan can suggest Gabbro from a photo and surface these checks on the result card.

What is Gabbro made of?

Gabbro composition: Plagioclase + pyroxene ± olivine (basalt chemistry). It forms via slow cooling of mafic magma at depth and is found in Layered intrusions, ophiolites, oceanic crust Layer 3.

Is Gabbro valuable?

Dimension stone and aggregate; ore-hosting gabbros valued for mineralization.