
mineral
Green Quartz (Prasiolite/Adventurine/Jasper)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Pale to deep green, Luster: Vitreous (glassy) to waxy, Crystal Structure: Hexagonal/Trigonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Pale to deep green, Luster: Vitreous (glassy) to waxy, Crystal Structure: Hexagonal/Trigonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins, volcanic cavities, or metamorphic rocks. Most natural green quartz is associated with areas where silicon-rich fluids were present during geological shifts.
Uses & applications
Used in gemstone production for jewelry (rings, pendants), as decorative ornamental stones, and highly valued by mineral collectors and 'crystal healing' practitioners.
Geological facts
Natural green quartz (Prasiolite) is extremely rare in nature; most commercial green quartz is produced by heat-treating amethyst. Green quartz with inclusions is often called Aventurine.
Field identification & locations
Identify by its ability to scratch glass (hardness 7) and its characteristic conchoidal (shell-like) fracture. Commonly found in Brazil, Russia, and portions of the USA like Arizona.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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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)
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Septarian Pebble
Septarian nodule / Concretion
sedimentary