Rock Identifier
Quartz (Golden Quartz / Citrine / Iron-stained Quartz) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (Golden Quartz / Citrine / Iron-stained Quartz)

Silicon Dioxide (SiO2)

Mohs hardness of 7, glassy to vitreous luster, conchoidal fracture, hexagonal crystal system, transparent to translucent with pale yellow-gold staining

Identified More mineral
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Physical properties

Mohs hardness of 7, glassy to vitreous luster, conchoidal fracture, hexagonal crystal system, transparent to translucent with pale yellow-gold staining

Formation & geological history

Formed in igneous pegmatites, hydrothermal veins, and metamorphic rocks. Golden hues often come from iron inclusions or natural radiation.

Uses & applications

Popular for crystal collecting, lapidary projects, metaphysical practices, and gemstone jewelry.

Geological facts

Quartz is one of the most abundant minerals on Earth's continental crust. Pure quartz is clear, but trace elements create a vast array of colorful varieties.

Field identification & locations

Identified by its ability to easily scratch glass (Mohs 7), lack of cleavage, vitreous luster, and typical conchoidal fracture patterns. Commonly found worldwide.