mineral

Orange Quartz

Silicon Dioxide (SiO2) with Hematite inclusions

Hardness: 7 (Mohs scale); Color: Pale orange to peachy pink; Luster: Vitreous to waxy (when weathered); Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.

Hardness: 7 (Mohs scale)
Color: Pale orange to peachy pink
Luster: Vitreous to waxy (when weathered)

Identified July 16, 2026More mineral →

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Physical properties

Formation & geological history

Formed in igneous and metamorphic environments, typically crystallizing from hydrothermal veins. The orange hue is caused by inclusions of iron oxides such as hematite or limonite during formation.

Uses & applications

Used primarily in lapidary arts, for ornamental carvings, pocket stones, and as metaphysical healing crystals. Industrial grade quartz is used in glassmaking and electronics.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. When the orange color is very deep and transparent, it is officially classified as Citrine, but opaque or milky specimens are generally called Orange Quartz.

Field identification & locations

Identify in the field by its hardness (it will scratch glass) and lack of cleavage. It is found globally, with major deposits in Brazil and Madagascar. Collectors look for clarity and vibrant saturation.

Other mineral specimens

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Sandstone (with potential mineral staining/concretions)

Arenite (SiO2 based)

sedimentary

Sandstone with Mineral Veining or Crust

Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)

sedimentary

Schist

Metamorphic

Potassium Feldspar (Orthoclase)

Orthoclase (KAlSi3O8)

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Gypsum (variety Selenite or Alabaster)

Calcium sulfate dihydrate (CaSO4·2H2O)

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Nephrite Jade

Nephrite

Mineral/Rock