mineral
Quartz (Rose Quartz)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale, pale pink to rose-red color, vitreous to greasy luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, pale pink to rose-red color, vitreous to greasy luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65.
Formation & geological history
Forms in pegmatites, hydrothermal veins, and metamorphic environments through the cooling of silica-rich solutions or magmas over geological timescales.
Uses & applications
Used widely in ornamental carvings, gemstone jewelry, holistic and metaphysical practices, and occasionally in optical components.
Geological facts
The pink coloration is typically caused by trace amounts of titanium, iron, or manganese, or microscopic inclusions of dumortierite.
Field identification & locations
Easily identified by its distinct pink color, lack of cleavage, and high hardness which scratches glass. Found globally, notably in Brazil, Madagascar, and the USA.
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Soil with Mineral Detritus and Quartz Fragments
Regolith / Silicate Mineral Aggregate
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Limonite / Goethite (Iron Ore Mineral nodule)
FeO(OH)·nH2O / FeO(OH)
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Septarian Pebble
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Schist
Schist
Metamorphic