
mineral
Rose Quartz with Schist Matrix
Silicon Dioxide (SiO2) with Mica-Schist
AI-generated identification · may be incorrectHardness: 7 (Quartz) / 2-3 (Mica); Color: Pale pink to lavender with dark grey/black flecked matrix; Luster: Vitreous to greasy on quartz faces, pearly/metallic on schist; Crystal System: Hexagonal; Cleavage: None (conchoidal fracture).
- Hardness
- 7 (Quartz) / 2-3 (Mica)
- Color
- Pale pink to lavender with dark grey/black flecked matrix
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Physical properties
Hardness: 7 (Quartz) / 2-3 (Mica); Color: Pale pink to lavender with dark grey/black flecked matrix; Luster: Vitreous to greasy on quartz faces, pearly/metallic on schist; Crystal System: Hexagonal; Cleavage: None (conchoidal fracture).
Formation & geological history
Formed in igneous pegmatites or hydrothermal veins under high pressure and temperature. The pink color is often attributed to microscopic inclusions of dumortierite or manganese.
Uses & applications
Commonly used for lapidary work, decorative ornamental carvings, crystal healing collections, and as an ore of silica.
Geological facts
Rose quartz is unique because it rarely forms distinct crystals with faces; instead, it usually grows in massive, irregular lumps. The dark material attached is likely a mica-schist matrix common in many pegmatitic environments.
Field identification & locations
Identify by its characteristic pink hue and its ability to scratch glass (hardness 7). It is commonly found in Brazil, Madagascar, and the Black Hills of South Dakota. Collectors should look for depth of color and clarity.
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