Rock Identifier
Dark gray crystalline rock, likely diorite or gabbro (Coarse-grained mafic/intermediate intrusive rock; commonly plagioclase feldspar + amphibole/pyroxene, with possible biotite) — igneous
igneous

Dark gray crystalline rock, likely diorite or gabbro

Coarse-grained mafic/intermediate intrusive rock; commonly plagioclase feldspar + amphibole/pyroxene, with possible biotite

AI-generated identification · may be incorrect

Hardness about 6–7 Mohs; dark gray, granular texture, subvitreous to dull luster, interlocking crystals, and no obvious cleavage as a whole rock. The photograph cannot reliably distinguish diorite from gabbro or amphibolite.

Identified More igneous
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Physical properties

Hardness about 6–7 Mohs; dark gray, granular texture, subvitreous to dull luster, interlocking crystals, and no obvious cleavage as a whole rock. The photograph cannot reliably distinguish diorite from gabbro or amphibolite.

Formation & geological history

Formed when magma slowly cooled beneath Earth’s surface, producing visible crystals; typically Paleozoic to Precambrian in exposed terrains, though intrusive bodies occur throughout geologic time.

Uses & applications

Used as crushed aggregate, road base, riprap, building stone, and occasionally countertops or decorative stone; ordinary hand specimens have little commercial value.

Geological facts

Diorite is intermediate in composition, whereas darker gabbro is compositionally equivalent to basalt but coarse-grained. Surface weathering and lighting can make either appear nearly black.

Field identification & locations

Look for interlocking light plagioclase and dark amphibole/pyroxene grains; a fresh broken surface is more diagnostic than the weathered exterior. Common worldwide in plutons and continental mountain belts.