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

Red Jasper

Silicon Dioxide (SiO2) with Hematite inclusions

Hardness: 6.5-7 (Mohs scale), Color: Brick red to brownish-red, Luster: Dull to vitreous, Crystal Structure: Microcrystalline/Cryptocrystalline (Trigonal), Cleavage: None/Conchoidal fracture, 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: Dull to vitreous, Crystal Structure: Microcrystalline/Cryptocrystalline (Trigonal), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.58-2.91

Formation & geological history

Formed through the deposition of silica from water-rich environments, often in hydrothermal veins or as a secondary replacement mineral in volcanic or sedimentary beds. The red color is caused by high concentrations of iron oxide (hematite).

Uses & applications

Widely used as a gemstone in jewelry (cabochons, beads), decorative carvings, lapidary art, and occasionally as a minor industrial abrasive.

Geological facts

Red Jasper has been used by humans for millennia; it was known as the 'rain-bringer' in ancient cultures and was famously used in the breastplate of the high priest in biblical times.

Field identification & locations

Identify by its deep red color, high hardness (will scratch glass), and smooth, conchoidal (shell-like) fracture pattern. It is commonly found in gravel beds, river banks, and desert environments worldwide, particularly in the US, Brazil, and India.