
mineral
Hematoid Quartz
Silicon Dioxide with Hematite inclusions (SiO2 + Fe2O3)
AI-generated identification · may be incorrectHardness of 7 on the Mohs scale, pale pink to clear crystal matrix with distinct reddish-brown inclusions of hematite, vitreous luster, trigonal crystal system, conchoidal fracture, and no true cleavage. Specific gravity is approximately 2.65.
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Physical properties
Hardness of 7 on the Mohs scale, pale pink to clear crystal matrix with distinct reddish-brown inclusions of hematite, vitreous luster, trigonal crystal system, conchoidal fracture, and no true cleavage. Specific gravity is approximately 2.65.
Formation & geological history
Formed in hydrothermal veins and pegmatites where silica-rich fluids crystallized in the presence of iron oxide minerals, trapping hematite within or upon the quartz structures during various geological eras.
Uses & applications
Used primarily in lapidary arts, metaphysical and healing practices, and as a popular specimen for mineral collectors and jewelry making.
Geological facts
Hematoid quartz is often referred to as 'fire quartz' or 'red quartz' due to the striking contrast between the translucent quartz and the blood-red iron oxide inclusions. It is believed by crystal practitioners to ground and balance energies.
Field identification & locations
Easily identified by its glass-like quartz appearance combined with distinct rust-red or hematite staining. Commonly found in locations with rich iron and quartz deposits such as Brazil, Madagascar, and parts of the United States.
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Sandstone (with potential mineral staining/concretions)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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