Rock Identifier
Tumbled jasper or quartzite pebble (Jasper (microcrystalline quartz, SiO₂), possibly iron-stained quartzite) — metamorphic
metamorphic

Tumbled jasper or quartzite pebble

Jasper (microcrystalline quartz, SiO₂), possibly iron-stained quartzite

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; opaque cream-yellow with pink-red hematite/iron-oxide veining, waxy to dull luster, and no visible cleavage. Fine-grained, compact texture; exact identification requires hardness and streak tests.

Identified More metamorphic
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Physical properties

Hardness about 6.5–7 Mohs; opaque cream-yellow with pink-red hematite/iron-oxide veining, waxy to dull luster, and no visible cleavage. Fine-grained, compact texture; exact identification requires hardness and streak tests.

Formation & geological history

Likely formed from silica-rich sediment or volcanic material later silicified and/or metamorphosed, with iron-oxide staining along fractures. Such rocks range from Precambrian to much younger and occur in many continental environments.

Uses & applications

Used as a lapidary material for tumbled stones, cabochons, carvings, and decorative objects; common pieces have modest value.

Geological facts

The rounded shape and smooth surface indicate natural water abrasion or commercial tumbling. Red and yellow colors commonly result from hematite and goethite impurities.

Field identification & locations

Commonly found in stream gravels and jasper/quartzite deposits worldwide; it should scratch glass but not be scratched by a steel knife. A streak test, specific gravity, and close inspection for quartz grains would distinguish jasper from quartzite.