
mineral
Rose Quartz
Silicon Dioxide (SiO2)
Mohs hardness of 7, pale pink to rose-red color, vitreous to greasy luster, trigonal crystal system, no true cleavage, conchoidal fracture, translucent to sub-translucent.
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Physical properties
Mohs hardness of 7, pale pink to rose-red color, vitreous to greasy luster, trigonal crystal system, no true cleavage, conchoidal fracture, translucent to sub-translucent.
Formation & geological history
Forms primarily in pegmatites, hydrothermal veins, and igneous rocks through the slow cooling of silica-rich magma. The pink coloration is typically due to microscopic inclusions of trace fibrous minerals like dumortierite.
Uses & applications
Used extensively in lapidary work, jewelry, ornamental carvings, beads, polished stones, and highly prized by crystal and mineral collectors.
Geological facts
Unlike many other quartz varieties, rose quartz rarely forms distinct, well-defined crystal faces. Specimens showing well-developed crystal faces are extremely rare and known as crystalline rose quartz or pink quartz.
Field identification & locations
Identified by its distinctive pale pink color, vitreous luster, and hardness (scratches glass readily). Frequently found in Brazil, Madagascar, South Africa, and the United States (South Dakota).
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Septarian Pebble
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Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
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Potassium Feldspar (Orthoclase)
Orthoclase (KAlSi3O8)
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Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral