Rock Identifier
Quartz on Basalt (Silicon Dioxide (SiO2) on Mafic Igneous Rock) — Mineral on Igneous Rock
Mineral on Igneous Rock

Quartz on Basalt

Silicon Dioxide (SiO2) on Mafic Igneous Rock

Hardness: 7 (quartz), 5-6 (basalt); Color: White/clear crystals on dark gray/black host rock; Luster: Vitreous to pearly crystals; Structure: Hexagonal crystals on a fine-grained crystalline matrix.

Hardness
7 (quartz), 5-6 (basalt)
Color
White/clear crystals on dark gray/black host rock
Luster
Vitreous to pearly crystals
Identified More mineral on igneous rock

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Physical properties

Hardness: 7 (quartz), 5-6 (basalt); Color: White/clear crystals on dark gray/black host rock; Luster: Vitreous to pearly crystals; Structure: Hexagonal crystals on a fine-grained crystalline matrix.

Formation & geological history

Formed through hydrothermal precipitation where silica-rich fluids filled cavities (vesicles) or cracks in cooling volcanic basaltic lava flows.

Uses & applications

Commonly used for geological study, teaching specimens, and minor decorative items or aquarium stone.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. When it grows inside the gas bubbles of basalt, it can eventually form geodes if the pocket is large enough.

Field identification & locations

Identify in the field by the contrast between a dark, heavy, fine-grained rock and white, hard crystals that can scratch glass. Often found in volcanic regions.