
mineral
Likely tumbled rose quartz
Quartz, SiO₂ (pink variety commonly called rose quartz)
AI-generated identification · may be incorrectSmall, polished, elongated pebble with pale pink to lilac color and a vitreous-to-waxy sheen. Quartz has Mohs hardness 7, a trigonal crystal structure, no cleavage, and uneven to conchoidal fracture; the photo alone cannot confirm its identity.
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Physical properties
Small, polished, elongated pebble with pale pink to lilac color and a vitreous-to-waxy sheen. Quartz has Mohs hardness 7, a trigonal crystal structure, no cleavage, and uneven to conchoidal fracture; the photo alone cannot confirm its identity.
Formation & geological history
Rose quartz forms in pegmatites and hydrothermal veins as silica-rich fluids cool; its pink color is associated with trace elements or microscopic inclusions. Such deposits range from Precambrian to geologically recent.
Uses & applications
Used for beads, cabochons, carvings, and inexpensive ornamental objects; this small tumbled piece is mainly decorative or collectible.
Geological facts
Quartz is one of Earth’s most abundant minerals, and tumbling rounds its edges and brings out a smooth polish.
Field identification & locations
Check for glassy luster, hardness near 7, and lack of cleavage; rose quartz commonly occurs in Brazil, Madagascar, India, and the United States. The image suggests a polished specimen but is not enough to distinguish quartz from dyed stone or glass.
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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
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Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary