mineral

Strawberry Quartz (Quartz with Hematite inclusions)

Silicon Dioxide with Iron Oxide (SiO2 + Fe2O3)

Hardness: 7 Mohs; Color: Transparent with reddish-pink flecks or streaks; Luster: Vitreous; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Hardness: 7 Mohs
Color: Transparent with reddish-pink flecks or streaks
Luster: Vitreous

Identified June 9, 2026More mineral →

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Physical properties

Hardness: 7 Mohs; Color: Transparent with reddish-pink flecks or streaks; Luster: Vitreous; Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Formation & geological history

Formed in igneous and metamorphic environments where iron minerals like hematite or lepidocrocite are present during the crystallization of quartz.

Uses & applications

Primarily used for lapidary work, jewelry making (beads, cabochons), and as a collector's specimen. It is also popular in holistic and metaphysical communities.

Geological facts

The 'strawberry' appearance is caused by tiny needle-like inclusions of iron oxide. It is often confused with Rose Quartz, which gets its color from different trace elements and usually lacks distinct visible flakes.

Field identification & locations

Identify by looking for characteristic red or pink speckling within a clear or cloudy quartz matrix. Commonly found in Russia, Kazakhstan, and Brazil. It should be able to scratch glass.

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