
mineral
Rose Quartz
Rose Quartz (SiO₂)
Hardness: 7 (Mohs scale), Color: Pink (ranging from very pale pink to deep rose), Luster: Vitreous to waxy, Crystal structure: Hexagonal (usually massive or anhedral, rarely forms distinct crystals), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Pink (ranging from very pale pink to deep rose), Luster: Vitreous to waxy, Crystal structure: Hexagonal (usually massive or anhedral, rarely forms distinct crystals), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Rose Quartz forms primarily during the hydrothermal stage of pegmatite formation or in quartz veins. It can also be found in high-temperature hydrothermal deposits. The distinctive pink color is believed to be caused by trace amounts of titanium, iron, or manganese, or by microscopic inclusions of dumortierite. Geological age varies widely depending on the formation event, typically associated with the crystallization of igneous and metamorphic rocks.
Uses & applications
Rose quartz is widely used in jewelry (cabochons, beads, carvings), ornamental objects, and as a popular collector's mineral. In spirituality and new age practices, it's often referred to as the 'love stone' and associated with healing and emotional well-being.
Geological facts
Massive rose quartz is often found in large quantities, making it relatively affordable. Fine crystalline rose quartz is much rarer. The best quality rose quartz with excellent transparency and color intensity is highly prized. Some specimens can exhibit asterism (a star-like effect) when cut as cabochons, though this is rare.
Field identification & locations
Rose quartz is identified by its characteristic pink color and vitreous to waxy luster. Its hardness (7) means it can scratch glass and most metals. It usually occurs in massive, anhedral forms, not well-defined crystals. It's commonly found in Brazil (Minas Gerais), South Dakota (USA), Madagascar, India, and Sri Lanka. In the field, look for milky to transparent pink masses in pegmatites and quartz veins. Collectors should look for good color saturation and minimal inclusions.
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