Rock Identifier
Rose Quartz (Silicon Dioxide (SiO2) with trace amounts of titanium, iron, or manganese) — mineral
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)
Identified More mineral

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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.