
mineral
Red jasper
Jasper, an opaque microcrystalline variety of quartz (SiO₂), colored mainly by iron oxides
AI-generated identification · may be incorrectTypically Mohs hardness 6.5–7, opaque brick-red to reddish-brown, with a dull to waxy luster and cryptocrystalline quartz structure; no visible cleavage, conchoidal to uneven fracture, and density about 2.5–2.7.
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Physical properties
Typically Mohs hardness 6.5–7, opaque brick-red to reddish-brown, with a dull to waxy luster and cryptocrystalline quartz structure; no visible cleavage, conchoidal to uneven fracture, and density about 2.5–2.7.
Formation & geological history
Forms when silica-rich fluids cement or replace fine sediments and volcanic material, with iron staining producing the red color; specimens commonly formed in Precambrian to younger hydrothermal and sedimentary environments.
Uses & applications
Used for beads, cabochons, carvings, countertops, and ornamental objects; modest jewelry and lapidary material.
Geological facts
Jasper is a variety of chalcedony or microcrystalline quartz, though its dense opaque texture distinguishes it from translucent agate. The pictured piece appears naturally fractured and rounded, possibly lightly tumbled or water-worn.
Field identification & locations
Identify by its uniform red color, opacity, fine grain, hardness, and lack of cleavage; common sources include India, Madagascar, Brazil, the United States, and Australia. A streak, hardness, and acid test can help distinguish it from red ceramic or dyed stone.
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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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary