Rock Identifier
Quartz (Milky or Yellow/Citrine Quartz) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (Milky or Yellow/Citrine Quartz)

Silicon Dioxide (SiO2)

Hardness of 7 on the Mohs scale, vitreous to greasy luster, translucent to opaque, conchoidal fracture with no true cleavage, hexagonal crystal system often appearing massive or tumbled in this form.

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Physical properties

Hardness of 7 on the Mohs scale, vitreous to greasy luster, translucent to opaque, conchoidal fracture with no true cleavage, hexagonal crystal system often appearing massive or tumbled in this form.

Formation & geological history

Formed in a wide variety of geological environments including igneous, metamorphic, and sedimentary rocks. Often crystallizes from silica-rich hydrothermal veins and pegmatites.

Uses & applications

Used in electronics, oscillators, glassmaking, abrasives, gemstone carving, and mineral specimen collecting.

Geological facts

Quartz is one of the most abundant and widely distributed minerals on Earth's continental crust. Given the regional prior near Karnataka/Andhra Pradesh in India, quartz and pegmatitic minerals are extremely common in the local Dharwar craton geology.

Field identification & locations

Easily identified by its hardness (scratches glass), lack of cleavage, and conchoidal fracture. Common in river gravels and weathered outcrops.