Rock Identifier
Milky Quartz (Gold-bearing Prospecting Specimen) (Silicon Dioxide (SiO2)) — mineral
mineral

Milky Quartz (Gold-bearing Prospecting Specimen)

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Translucent white to milky white with iron oxidation/rust staining (ochre); Luster: Vitreous (glassy) to greasy; Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Hardness
7 on Mohs scale
Luster
Vitreous (glassy) to greasy
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Translucent white to milky white with iron oxidation/rust staining (ochre); Luster: Vitreous (glassy) to greasy; Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed in hydrothermal veins where silica-rich fluids are injected into fractures in the surrounding host rock. Commonly found in orogenic belts. This specimen shows surface weathering indicating it was likely found in a riverbed or surface deposit (alluvial or eluvial).

Uses & applications

Used industrially in glass making, electronics (piezoelectric properties), and as an abrasive. In this form, it is primarily a geological specimen or ore sample for gold prospecting.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Specimens like this one, showing heavy iron staining and 'rotten' pockets, are historically used by prospectors as an indicator of potential gold mineralization.

Field identification & locations

Identify in the field by its inability to be scratched by a steel knife, its lack of cleavage planes, and its characteristic milky appearance. Found globally, especially in mountainous or volcanic regions. Tip: Look for 'vuggy' or pitted textures which may have once housed other minerals.