Quartz with Hematite Inclusions
Silicon Dioxide (SiO2) with Ferric Oxide (Fe2O3)
Rock Type: mineral

Physical Properties
Hardness: 7 (Quartz) and 5.5-6.5 (Hematite). Color: White/translucent base with reddish-brown or rusty spots. Luster: Vitreous to dull. Crystal structure: Trigonal/Hexagonal. Cleavage: Indistinct.
Formation & Geological History
Formed in hydrothermal veins or as a secondary mineral deposit where iron-rich fluids interact with cooling silica-rich solutions. Often found in Precambrian formations but can occur in various geological ages.
Uses & Applications
Primary use as collector specimens, decorative lapidary work (cabochons), and sometimes used in metaphysical healing practices. The hematite content is generally too low for industrial iron ore extraction.
Geological Facts
The reddish-brown color is caused by minute particles of hematite trapped within the quartz crystal lattice during its growth, or as a coating in cracks within the stone. In its crystalline form, this is often called 'Ferruginous Quartz'.
Field Identification & Locations
Identify in the field by checking for the hardness of quartz (cannot be scratched by a steel blade) and the characteristic rusty-red color that doesn't wash off. Commonly found in areas with metamorphic activity or near iron ore deposits.
Identified on: 4/25/2026
Mode: Standard