Rock Identifier
Quartz-bearing dark mineral specimen, likely schorl tourmaline in quartz (Quartz (SiO₂) with probable schorl tourmaline (NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄)) — mineral
mineral

Quartz-bearing dark mineral specimen, likely schorl tourmaline in quartz

Quartz (SiO₂) with probable schorl tourmaline (NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄)

AI-generated identification · may be incorrect

Uneven white-to-honey quartz with a black, granular to prismatic inclusion or attached mass. Quartz has Mohs hardness 7, vitreous luster, no cleavage, and hexagonal crystal structure; schorl is typically Mohs 7–7.5 with three-sided prismatic crystals and poor cleavage.

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Physical properties

Uneven white-to-honey quartz with a black, granular to prismatic inclusion or attached mass. Quartz has Mohs hardness 7, vitreous luster, no cleavage, and hexagonal crystal structure; schorl is typically Mohs 7–7.5 with three-sided prismatic crystals and poor cleavage.

Formation & geological history

Likely formed in a granitic pegmatite or hydrothermal vein, where boron-rich fluids crystallized black tourmaline with quartz during late-stage cooling, generally in Phanerozoic continental crust.

Uses & applications

Quartz is used in glass, abrasives, electronics, and decorative stone; black tourmaline is a popular collector mineral and gemstone. This small rough specimen has modest commercial value.

Geological facts

The black material may alternatively be biotite, hornblende, or another dark silicate; a definitive identification requires close inspection or testing. Tourmaline is strongly piezoelectric and can become electrically charged when heated or compressed.

Field identification & locations

Look for glassy quartz that scratches steel and does not fizz in dilute acid, plus black tourmaline’s elongated striated prisms; common sources include Brazil, Afghanistan, Madagascar, and the United States. Estimated value: $3–$15 for a typical small specimen, higher if well-crystallized.