
mineral
Red jasper
Jasper, microcrystalline quartz (SiO₂) colored mainly by iron oxides
AI-generated identification · may be incorrectTypically opaque brick-red to brown, with a vitreous-to-dull luster; hardness about 6.5–7 Mohs, no cleavage, and conchoidal fracture. The rounded, glossy surface indicates a tumbled and polished specimen.
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Physical properties
Typically opaque brick-red to brown, with a vitreous-to-dull luster; hardness about 6.5–7 Mohs, no cleavage, and conchoidal fracture. The rounded, glossy surface indicates a tumbled and polished specimen.
Formation & geological history
Forms when silica-rich fluids cement or replace sediment and volcanic material, with iron oxides producing the red color. Deposits occur in many ages, commonly associated with volcanic or hydrothermal environments.
Uses & applications
Used for cabochons, beads, carvings, ornaments, and polished lapidary pieces; occasionally as decorative stone. Common material generally has modest value.
Geological facts
Jasper is a variety of chalcedony or microcrystalline quartz, though its opaque, fine-grained texture distinguishes it from translucent agate. Color zoning, veining, or brecciated patterns can increase desirability.
Field identification & locations
Identify by its opaque red color, very fine texture, glassy polish, and inability to scratch with a copper coin; it should scratch glass, though testing a polished piece may damage it. Common sources include India, Madagascar, Brazil, Australia, and the western United States.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous