
mineral
Rose Quartz
Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese
Hardness: 7 on Mohs scale; Color: pale pink to rose red; Luster: vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: none (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- pale pink to rose red
- Luster
- vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: pale pink to rose red; Luster: vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: none (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed in late-stage cooling of magmatic pegmatites (coarse-grained igneous rocks) or in hydrothermal veins. Can be found in Precambrian and younger geological formations.
Uses & applications
Extensively used in lapidary for carvings, beads, and cabochons. Significant in the metaphysical market for 'healing stones'. Historically used as an ornamental stone and occasionally in industrial applications as a source of high-purity silica.
Geological facts
Unlike اکثر other quartz varieties, Rose Quartz rarely forms distinct large crystal faces; it typically occurs as massive aggregates. Some specimens exhibit 'asterism' (a star effect) when polished into spheres or cabochons due to tiny rutile inclusions.
Field identification & locations
Identify by its characteristic pink hue and translucency. In the field, look for glassy, blocky masses within pegmatite veins. Major source locations include Brazil, South Africa, Madagascar, and the Black Hills of South Dakota, USA.
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