
mineral
Strawberry Quartz (Red Aventurine)
Silicon Dioxide (SiO2) with Hematite/Goethite inclusions
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Pinkish-red to reddish-brown, Luster: Vitreous, Crystal Structure: Trigonal (Hexagonal system), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Pinkish-red to reddish-brown, Luster: Vitreous, Crystal Structure: Trigonal (Hexagonal system), Specific Gravity: 2.65
Formation & geological history
Formed in hydrothermal veins or granitic pegmatites; the color comes from tiny inclusions of iron oxide minerals like lepidocrocite or hematite that occur during the crystallization of the quartz.
Uses & applications
Primarily used in jewelry, lapidary arts (carvings and cabochons), and by mineral collectors. It is also popular in holistic practices.
Geological facts
True Strawberry Quartz is quite rare and often confused with Red Aventurine, which contains mica inclusions. Many specimens on the market are actually master-melt glass (cherry quartz), but natural specimens show unique, needle-like mineral inclusions.
Field identification & locations
Identify by looking for 'sparkles' or 'shimmer' (aventurescence) or distinct iron needle inclusions under magnification. Commonly found in Brazil, Russia, and Kazakhstan.
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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