Rock Identifier
Quartzite (Yellow/Tan river stone variety) (Quartzite (primarily SiO2)) — metamorphic
metamorphic

Quartzite (Yellow/Tan river stone variety)

Quartzite (primarily SiO2)

Hardness: 7 on Mohs scale (scratches glass). Color: Tan, yellowish-brown, or grey. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (microcrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.7.

Hardness
7 on Mohs scale (scratches glass)
Color
Tan, yellowish-brown, or grey
Luster
Vitreous to waxy
Identified More metamorphic

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Physical properties

Hardness: 7 on Mohs scale (scratches glass). Color: Tan, yellowish-brown, or grey. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (microcrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.7.

Formation & geological history

Formed from the metamorphism of quartz sandstone under intense heat and pressure, usually during mountain-building events. The rounded shape indicates significant water erosion/transport in a river or glacial environment.

Uses & applications

Used as a decorative stone in landscaping, a durable aggregate for construction, and historically as a material for stone tools or 'strike-a-lights' for fire making.

Geological facts

Quartzite is so durable that it often remains as resistant ridges or 'caprock' in mountain ranges long after softer rocks have eroded away. It is tougher than the sandstone from which it originated because the quartz grains have fused together.

Field identification & locations

Identify by its extreme hardness (cannot be scratched by a steel knife) and its grainy, 'sugary' texture on a fresh break. Common in riverbeds and glacial tills globally. It feels heavier and denser than common sandstone.