
metamorphic
Pale quartz-rich pebble (likely quartzite)
Quartzite; chiefly microcrystalline quartz (SiO₂), possibly with feldspar or iron-oxide staining
AI-generated identification · may be incorrectHardness about 7 Mohs, pale cream-yellow color, glassy to dull luster, granular interlocking texture, and no obvious cleavage; specific gravity roughly 2.6–2.7. The rounded, smooth surface indicates natural water abrasion or tumbling.
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Physical properties
Hardness about 7 Mohs, pale cream-yellow color, glassy to dull luster, granular interlocking texture, and no obvious cleavage; specific gravity roughly 2.6–2.7. The rounded, smooth surface indicates natural water abrasion or tumbling.
Formation & geological history
Formed when quartz-rich sandstone was recrystallized under heat and pressure, commonly during regional metamorphism; its exact geological age cannot be determined from the photograph. Yellow coloration likely comes from minor iron oxides or weathering.
Uses & applications
Used as aggregate, road stone, landscaping material, and decorative stone; attractive pieces may be polished, but this specimen appears common and unworked.
Geological facts
Quartzite is generally more resistant to weathering than its parent sandstone and commonly preserves a sugary, fused quartz texture rather than visible sand grains.
Field identification & locations
Identify it by its very high hardness, pale color, and inability to scratch with a steel knife; quartz-rich pieces can scratch glass. Common in metamorphic mountain belts and gravel deposits.
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