Rock Identifier
Jasper (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Jasper

Microcrystalline Quartz (SiO2)

Hardness of 6.5 to 7 on the Mohs scale, reddish-brown color due to iron oxide impurities, waxy to vitreous luster, cryptocrystalline structure, no cleavage (conchoidal fracture), specific gravity around 2.65.

Identified More sedimentary
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Physical properties

Hardness of 6.5 to 7 on the Mohs scale, reddish-brown color due to iron oxide impurities, waxy to vitreous luster, cryptocrystalline structure, no cleavage (conchoidal fracture), specific gravity around 2.65.

Formation & geological history

Formed through the silification of sedimentary or volcanic rocks where silica-rich fluids replace organic material or fill cavities, often in hydrothermal environments or ocean basins.

Uses & applications

Used primarily in lapidary arts, making cabochons, beads, ornamental carvings, and decorative jewelry.

Geological facts

Jasper has been used by ancient peoples since antiquity for talismans, seals, and primitive tools. Red jasper specifically gets its vibrant color from hematite inclusions.

Field identification & locations

Can be identified by its distinctive opacity, lack of cleavage, smooth conchoidal fracture, and hardness which easily scratches glass. Commonly found globally in riverbeds, alluvial deposits, and volcanic regions.