
mineral
Rose Quartz
Quartz (Silicon Dioxide - SiO2)
Hardness: 7 on Mohs scale; Color: Pale pink to rose red; Luster: Vitreous/glassy; Crystal Structure: Trigonal (often found as massive habit); Cleavage: Poor/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: Trigonal (often found as massive habit); Cleavage: Poor/none (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed at high temperatures in deep-seated igneous pegmatites or hydrothermal veins. The color is derived from trace amounts of titanium, iron, or manganese. Specimens in the Ohio region are often glacial erratics transported south from the Canadian Shield during the Ice Age.
Uses & applications
Predominantly used for ornamental carvings, semi-precious jewelry (beads and cabochons), and as a popular lapidary material for hobbyists and collectors.
Geological facts
Unlike other varieties of quartz, rose quartz rarely forms well-defined crystal faces and is most commonly found in shapeless irregular masses. It is often cited as the 'stone of unconditional love' in metaphysical circles.
Field identification & locations
In Ohio, look for it in gravel pits or glacial till. Identification involves its distinct pink translucency and its ability to scratch glass (hardness test). Its conchoidal fracture (shell-like curves) is a key visual indicator.
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