Rock Identifier
Rounded metamorphic pebble, likely quartzite or gneiss (Quartz-rich metamorphic rock; possibly foliated quartzite or gneiss) — metamorphic
metamorphic

Rounded metamorphic pebble, likely quartzite or gneiss

Quartz-rich metamorphic rock; possibly foliated quartzite or gneiss

AI-generated identification · may be incorrect

Light gray, fine- to medium-grained, rounded and naturally weathered; subdued satin to dull luster with faint wavy banding. Likely hardness around Mohs 6.5–7 if quartz-rich, with no obvious cleavage and moderate-to-high specific gravity (~2.6–2.7).

Identified More metamorphic
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Physical properties

Light gray, fine- to medium-grained, rounded and naturally weathered; subdued satin to dull luster with faint wavy banding. Likely hardness around Mohs 6.5–7 if quartz-rich, with no obvious cleavage and moderate-to-high specific gravity (~2.6–2.7).

Formation & geological history

Probably formed when quartz-rich sandstone or granitic material was subjected to substantial heat and pressure, then eroded into a smooth pebble by water or glacial transport. Precise geological age and identification require a fresh broken surface or testing.

Uses & applications

Commonly used as landscaping stone, aggregate, or decorative/tumbled material; generally little jewelry value unless it displays attractive banding or unusual mineralization.

Geological facts

The rounded shape reflects abrasion during transport, while the subtle streaks may indicate foliation, compositional layering, or surface weathering. A glass-scratch test can help distinguish quartz-rich rock from softer limestone or concrete.

Field identification & locations

Common in streambeds, beaches, glacial deposits, and areas underlain by quartzite or metamorphic basement rocks. Test whether it scratches glass and examine a fresh surface for interlocking quartz grains; acid testing and a close inspection are needed to exclude marble or concrete.