Rock Identifier
Red Jasper (Silicon Dioxide (Microcrystalline Quartz), SiO2) — sedimentary
sedimentary

Red Jasper

Silicon Dioxide (Microcrystalline Quartz), SiO2

Hardness of 6.5 to 7 on the Mohs scale, opaque reddish-brown to brick-red color due to iron oxide inclusions, waxy to vitreous luster, microcrystalline (cryptocrystalline) crystal structure, conchoidal fracture with no true cleavage, specific gravity of 2.58 to 2.91.

Identified More sedimentary
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Physical properties

Hardness of 6.5 to 7 on the Mohs scale, opaque reddish-brown to brick-red color due to iron oxide inclusions, waxy to vitreous luster, microcrystalline (cryptocrystalline) crystal structure, conchoidal fracture with no true cleavage, specific gravity of 2.58 to 2.91.

Formation & geological history

Formed through the hydrothermal deposition of silica-rich fluids or precipitation from silica-rich marine waters, often accumulating on ocean floors alongside iron-rich sedimentary deposits. Geological age varies widely depending on the deposit, ranging from Precambrian banded iron formations to younger hydrothermal veins.

Uses & applications

Widely used for tumbled stones, cabochons, carvings, ornamental objects, beads, and metaphysical crystal healing practices.

Geological facts

Jasper has been prized since ancient times as a sacred and protective stone, famously used by ancient Egyptians, Greeks, and Romans for talismans, seals, and signet rings.

Field identification & locations

Easily identified by its deep reddish-brown opaque appearance and waxy polish. It does not scratch with a steel knife due to its high quartz hardness. Found worldwide, with major deposits in India, Brazil, Russia, Australia, and the United States.