
mineral
Rose quartz
Quartz, silicon dioxide (SiO₂), variety rose quartz
AI-generated identification · may be incorrectMohs hardness 7; pale pink, translucent, with a vitreous luster and no cleavage. Trigonal crystal structure; often occurs as massive material rather than distinct crystals.
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Physical properties
Mohs hardness 7; pale pink, translucent, with a vitreous luster and no cleavage. Trigonal crystal structure; often occurs as massive material rather than distinct crystals.
Formation & geological history
Forms in silica-rich pegmatites and hydrothermal veins as magma cools and mineral-rich fluids crystallize. Its age depends on the deposit, commonly hundreds of millions to billions of years.
Uses & applications
Used for beads, carvings, ornaments, and decorative stone; rarely cut as a gemstone because it is usually translucent and massive.
Geological facts
The pink color is generally attributed to microscopic mineral inclusions or trace elements, depending on the specimen.
Field identification & locations
Common sources include Brazil, Madagascar, India, and South Africa. Identify it by its pink color, glassy fracture, hardness, and lack of cleavage; the image alone cannot confirm the variety.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary