Rock Identifier
Ruby in Quartz with Tourmaline (Corundum (Al2O3) in Silicon Dioxide (SiO2) with Schorl) — metamorphic
metamorphic

Ruby in Quartz with Tourmaline

Corundum (Al2O3) in Silicon Dioxide (SiO2) with Schorl

Hardness: Quartz (7), Ruby (9); Color: White/clear matrix with pink/red crystals; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Indistinct; SG: 2.65 - 4.0

Hardness
Quartz (7), Ruby (9)
Color
White/clear matrix with pink/red crystals
Luster
Vitreous to greasy
Identified More metamorphic

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Physical properties

Hardness: Quartz (7), Ruby (9); Color: White/clear matrix with pink/red crystals; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Indistinct; SG: 2.65 - 4.0

Formation & geological history

Formed through high-grade regional metamorphism or in hydrothermal veins and pegmatites where aluminum-rich fluids crystallize within silica-rich environments.

Uses & applications

Primarily used for mineral collecting, metaphysical purposes, and occasionally carved into decorative or ornamental items.

Geological facts

While Rubies are typically found in marble or basalt, finding them embedded in massive quartz is rarer and indicates a specific chemical environment rich in both alumina and silica.

Field identification & locations

Identify by the red hexagonal crystal shapes (rubies) embedded in a translucent white matrix. Commonly found in Madagascar, India, and parts of East Africa.