
mineral
Milky quartz with iron-oxide staining
Quartz (SiO₂), likely massive to crystalline vein quartz
AI-generated identification · may be incorrectWhite to translucent, vitreous luster, with rusty brown iron-oxide coatings and inclusions. Mohs hardness 7; trigonal crystal system, no cleavage, uneven to conchoidal fracture; specific gravity about 2.65.
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Physical properties
White to translucent, vitreous luster, with rusty brown iron-oxide coatings and inclusions. Mohs hardness 7; trigonal crystal system, no cleavage, uneven to conchoidal fracture; specific gravity about 2.65.
Formation & geological history
Quartz commonly precipitates from silica-rich fluids in fractures and veins, then may acquire iron-oxide staining during weathering. The image alone cannot establish its geological age or precise formation setting.
Uses & applications
Quartz is used in glassmaking, electronics, abrasives, and decorative stone; attractive pieces may be kept as inexpensive specimens.
Geological facts
The rusty material is likely iron oxides such as goethite or hematite, rather than part of the quartz crystal structure.
Field identification & locations
Identify by its glassy appearance, hardness (it scratches ordinary glass), and lack of cleavage; common in veins and weathered outcrops worldwide. The specimen appears to be quartz attached to rusty matrix.
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