Rock Identifier
Jasper and Quartz conglomerate (Silicon Dioxide (SiO2) with iron oxide impurities) — sedimentary
sedimentary

Jasper and Quartz conglomerate

Silicon Dioxide (SiO2) with iron oxide impurities

Hardness: 6.5-7 (Mohs scale), Color: Reddish-brown with white/translucent crystalline patches, Luster: Vitreous to dull, Crystal structure: Trigonal (microcrystalline/cryptocrystalline), Cleavage: None/Conchoidal fracture

Hardness
6
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 (Mohs scale), Color: Reddish-brown with white/translucent crystalline patches, Luster: Vitreous to dull, Crystal structure: Trigonal (microcrystalline/cryptocrystalline), Cleavage: None/Conchoidal fracture

Formation & geological history

Formed from silica-rich fluids precipitating in voids or cementing grains together within sedimentary environments, often colored by hematite (iron oxide). Found in various global deposits spanning from the Precambrian to Cenozoic eras.

Uses & applications

Commonly used for lapidary work, jewelry (cabochons), tumbling for decorative purposes, and as an ornamental stone due to its durability and color.

Geological facts

Jasper is a variety of chalcedony that owes its opacity and color to high levels of impurities. This specific piece shows a mixture of transparent quartz crystals and opaque red jasper.

Field identification & locations

Identify by its hardness (will scratch glass), varied opaque/translucent texture, and reddish coloration. Frequently found in riverbeds and glacial deposits. Common in regions like the Great Lakes or desert southwest USA.