Rock Identifier
Red Jasper (Silicon Dioxide with Hematite (SiO2 + Fe2O3)) — sedimentary
sedimentary

Red Jasper

Silicon Dioxide with Hematite (SiO2 + Fe2O3)

Hardness: 6.5-7 (Mohs scale), Color: Brick red to brownish-red, Luster: Vitreous to dull, Crystal Structure: Trigonal (microcrystalline), Cleavage: None, Specific Gravity: 2.58-2.91

Hardness
6
Identified More sedimentary

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Physical properties

Hardness: 6.5-7 (Mohs scale), Color: Brick red to brownish-red, Luster: Vitreous to dull, Crystal Structure: Trigonal (microcrystalline), Cleavage: None, Specific Gravity: 2.58-2.91

Formation & geological history

Formed through the deposition of silica-rich fluids in volcanic ash or sedimentary rocks. The red color comes from high concentrations of iron inclusions (Hematite) during the silicon dioxide's crystallization process.

Uses & applications

Used primarily for lapidary work, jewelry (cabochons and beads), ornamental carvings, and as a popular pocket stone for collectors.

Geological facts

Jasper was a favorite gem in the ancient world; its name can be traced back in Arabic, Persian, Hebrew, Assyrian, Greek, and Latin. It is often found in banded iron formations.

Field identification & locations

Identify by its opaque nature (unlike carnelian which is translucent), its smooth conchoidal fracture, and deep red streak. Commonly found in India, Brazil, USA, and South Africa.