Rock Identifier
Red Jasper (Silicon Dioxide (SiO2) with Iron Oxide inclusions) — sedimentary
sedimentary

Red Jasper

Silicon Dioxide (SiO2) with Iron Oxide inclusions

Hardness 6.5 to 7 on the Mohs scale. Brick red to terracotta brown color due to iron contents, dull to earthy or sub-vitreous luster, microcrystalline quartz structure with conchoidal fracture.

Identified More sedimentary
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Physical properties

Hardness 6.5 to 7 on the Mohs scale. Brick red to terracotta brown color due to iron contents, dull to earthy or sub-vitreous luster, microcrystalline quartz structure with conchoidal fracture.

Formation & geological history

Formed when microcrystalline silica solutions rich in iron oxides permeate volcanic ash, sediment, or hydrothermal veins, solidifying over time into microcrystalline chalcedony.

Uses & applications

Widely used in lapidary arts, jewelry making (cabochons, beads), decorative carvings, tumbling, and metaphysical stone collecting.

Geological facts

Red jasper has been used since ancient times in amulets and signet rings. Its distinct deep red coloration comes from hematite impurities finely distributed throughout the quartz matrix.

Field identification & locations

Identified by its rich opaque red-brown color, fine grain (no visible crystals to the naked eye), and high hardness (scratches glass). Common in quartz-rich sedimentary deposits and ancient volcanic regions worldwide.