Rock Identifier
Olivine Basalt (Mafic Volcanic Rock (rich in (Mg, Fe)2SiO4)) — igneous
igneous

Olivine Basalt

Mafic Volcanic Rock (rich in (Mg, Fe)2SiO4)

Hardness: 6-7 on Mohs scale. Color: Dark gray to black matrix with olive-green phenocrysts. Luster: Dull (matrix) to vitreous (crystals). Structure: Aphanitic with porphyritic texture. Specific gravity: 2.8-3.0.

Hardness
6-7 on Mohs scale
Color
Dark gray to black matrix with olive-green phenocrysts
Luster
Dull (matrix) to vitreous (crystals)
Identified More igneous

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Physical properties

Hardness: 6-7 on Mohs scale. Color: Dark gray to black matrix with olive-green phenocrysts. Luster: Dull (matrix) to vitreous (crystals). Structure: Aphanitic with porphyritic texture. Specific gravity: 2.8-3.0.

Formation & geological history

Formed from the rapid cooling of magnesium-rich and iron-rich lava at or near the Earth's surface. These specimens are typically associated with oceanic crust and volcanic hotspots.

Uses & applications

Used in construction as crushed stone or aggregate. High-quality olivine crystals (peridot) are used in jewelry. Also used as a flux in steel making.

Geological facts

Olivine is one of the first minerals to crystallize from a cooling magma. Some olivine-rich rocks (peridotites) originate from the Earth's mantle and are brought to the surface by volcanic eruptions.

Field identification & locations

Identify by looking for green, glassy 'grains' embedded in a dark, heavy rock. Found in volcanic regions like Hawaii, Iceland, and the Canary Islands. It is magnetic if high in iron content.