Rock Identifier
Quartz crystal cluster with dark tourmaline and iron staining (Quartz (SiO₂), likely with schorl tourmaline (NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄)) — mineral
mineral

Quartz crystal cluster with dark tourmaline and iron staining

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

AI-generated identification · may be incorrect

Appears to be a small natural crystal aggregate: translucent to milky quartz with vitreous luster, conchoidal fracture, and Mohs hardness 7, alongside a dark blue-black prismatic mineral possibly schorl tourmaline (Mohs 7–7.5); reddish-brown areas suggest iron-oxide staining or included garnet.…

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Physical properties

Appears to be a small natural crystal aggregate: translucent to milky quartz with vitreous luster, conchoidal fracture, and Mohs hardness 7, alongside a dark blue-black prismatic mineral possibly schorl tourmaline (Mohs 7–7.5); reddish-brown areas suggest iron-oxide staining or included garnet. Crystal form is likely hexagonal quartz with trigonal termination, though the image is not diagnostic.

Formation & geological history

Quartz–tourmaline-bearing pegmatites and hydrothermal veins formed from silica- and boron-rich fluids, commonly during late-stage igneous crystallization; age depends on locality, often Precambrian to Mesozoic.

Uses & applications

Primarily a collector specimen; clear quartz may be used for ornamental objects and electronics, while tourmaline is sometimes cut as a gemstone. Small irregular pieces generally have limited commercial value.

Geological facts

Quartz–tourmaline associations are characteristic of granitic pegmatites and can indicate chemically evolved magma systems.

Field identification & locations

Commonly found in pegmatites worldwide, including Brazil, Afghanistan, Madagascar, and the United States. Confirm with hardness, crystal habit, streak, and locality; a close photograph or testing is needed to distinguish tourmaline from other dark minerals.