Rock Identifier
Red Jasper (Opaque microcrystalline quartz (SiO2) with iron inclusions) — sedimentary
sedimentary

Red Jasper

Opaque microcrystalline quartz (SiO2) with iron inclusions

Hardness: 6.5-7 Mohs; Color: Brick red to brownish-red with occasional bands; Luster: Dull to waxy; Crystal Structure: Hexagonal (trigonal); Fracture: Conchoidal; Specific Gravity: 2.58-2.91

Hardness
6
Color
Brick red to brownish-red with occasional bands
Luster
Dull to waxy
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 Mohs; Color: Brick red to brownish-red with occasional bands; Luster: Dull to waxy; Crystal Structure: Hexagonal (trigonal); Fracture: Conchoidal; Specific Gravity: 2.58-2.91

Formation & geological history

Forms when fine-grained silica-rich sediments or volcanic ash are lithified. Its red color is derived from iron (hematite) inclusions that diffused through the silica during formation. Most common in ancient Precambrian or Phanerozoic deposits.

Uses & applications

Used extensively as a gemstone for jewelry (cabochons, beads), decorative carvings, lapidary art, and occasionally for metaphysical purposes.

Geological facts

Jasper is often found in massive form rather than distinct crystals. Because of its hardness, it was used in ancient times to create drills and scrapers. The name is derived from the Greek 'iaspis', meaning 'spotted stone'.

Field identification & locations

Identify by its deep red color, opacity (it will not let light through even at the edges), and smooth, waxy surface when worn by water. Found globally in areas with high silica and iron content, such as stream beds and coastal regions.