Rock Identifier
Quartz Sand Grain (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Quartz Sand Grain

Silicon Dioxide (SiO2)

AI-generated identification · may be incorrect

Hardness of 7 on the Mohs scale, clear to pale brown color, vitreous luster, hexagonal crystal system when well-formed, and conchoidal fracture with no true cleavage.

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Physical properties

Hardness of 7 on the Mohs scale, clear to pale brown color, vitreous luster, hexagonal crystal system when well-formed, and conchoidal fracture with no true cleavage.

Formation & geological history

Formed through the mechanical and chemical weathering of parent rocks like granite, accumulating in sedimentary environments like beaches and deserts over millions of years.

Uses & applications

Used in glass manufacturing, construction aggregates, electronics, and foundational geological studies of sediment transport.

Geological facts

Quartz is one of the most abundant and durable minerals on Earth's surface, resisting chemical weathering longer than almost any other mineral.

Field identification & locations

Identified by its high hardness, lack of cleavage, and resistance to acid; commonly found in sandstone formations and loose surface soils.