Rock Identifier
Quartzite / Quartz Geodeoid Nodules (Silicon Dioxide (SiO2)) — metamorphic
metamorphic

Quartzite / Quartz Geodeoid Nodules

Silicon Dioxide (SiO2)

Mohs hardness of 7, sugary to coarse crystalline texture, dull to vitreous luster, light brown to tan color with visible quartz grains. Very hard and resistant to scratching by steel.

Identified More metamorphic
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Physical properties

Mohs hardness of 7, sugary to coarse crystalline texture, dull to vitreous luster, light brown to tan color with visible quartz grains. Very hard and resistant to scratching by steel.

Formation & geological history

Formed by the metamorphism of quartz sandstone under high heat and pressure, or as secondary silica mineralizations forming nodules or geode exteriors in sedimentary strata.

Uses & applications

Used as construction aggregate, decorative landscaping stone, crushed stone for rail ballast, and as lapidary material if hollow with internal quartz crystals.

Geological facts

Quartzite is so durable that it resists chemical weathering and often forms prominent hills and ridges as surrounding rocks erode away.

Field identification & locations

Identified in the field by its extreme hardness (scratches glass) and sugary fracture surface where breaks occur through individual quartz grains rather than around them.