Rock Identifier
Gabbro (Gabbro (composed mainly of calcium-rich plagioclase feldspar and pyroxene)) — igneous
igneous

Gabbro

Gabbro (composed mainly of calcium-rich plagioclase feldspar and pyroxene)

Hardness: 6-7 on Mohs scale; Color: Dark gray to black, sometimes with a greenish tint; Luster: Dull to sub-vitreous; Crystal Structure: Phaneritic (coarse-grained, visible crystals); Specific Gravity: 2.7 to 3.3.

Hardness
6-7 on Mohs scale
Color
Dark gray to black, sometimes with a greenish tint
Luster
Dull to sub-vitreous
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale; Color: Dark gray to black, sometimes with a greenish tint; Luster: Dull to sub-vitreous; Crystal Structure: Phaneritic (coarse-grained, visible crystals); Specific Gravity: 2.7 to 3.3.

Formation & geological history

Formed through the slow cooling of magnesium-rich and iron-rich magma deep beneath the Earth's surface (intrusive). It is the plutonic equivalent of basalt and is commonly found in the oceanic crust and ophiolite complexes.

Uses & applications

Used widely as heavy-duty construction aggregate, road base, and crushed stone. High-quality specimens are polished and sold as 'black granite' for kitchen countertops, floor tiles, and cemetery headstones.

Geological facts

Gabbro makes up a large portion of the Earth's deep oceanic crust. It is often chemically and mineralogically identical to basalt, but it has much larger crystals because it cooled slower underground.

Field identification & locations

Identify in the field by its dark color and visible interlocking crystals that lack quartz. It is commonly found in mountainous regions where tectonic uplift has exposed deep-seated rocks. Collectors should look for 'Orbicular Gabbro' for unique patterns.