Rock Identifier
Red Jasper (possibly with Quartz or Hematite) (Silicon Dioxide (SiO2) with iron oxide impurities) — sedimentary or metamorphic
sedimentary or metamorphic

Red Jasper (possibly with Quartz or Hematite)

Silicon Dioxide (SiO2) with iron oxide impurities

Hardness: 6.5-7 (Mohs), Color: Opaque brick red to maroon, Luster: Vitreous to dull, Crystal Structure: Trigonal (microcrystalline), Fracture: Conchoidal, Specific Gravity: 2.58-2.91

Hardness
6
Identified More sedimentary or metamorphic
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Physical properties

Hardness: 6.5-7 (Mohs), Color: Opaque brick red to maroon, Luster: Vitreous to dull, Crystal Structure: Trigonal (microcrystalline), Fracture: Conchoidal, Specific Gravity: 2.58-2.91

Formation & geological history

Formed through the accumulation of fine-grained silica in sedimentary environments or as secondary fluids filling fractures in volcanic rock. The red color is caused by iron (hematite) inclusions within the cryptocrystalline quartz.

Uses & applications

Primarily used for lapidary work, jewelry (cabochons), carvings, and as a popular specimen for crystal healing and decorative collections.

Geological facts

Jasper is a variety of chalcedony. Historically, it was known as the 'supreme nurturer' and has been used in seals and amulets since ancient Mesopotamian and Greek times.

Field identification & locations

Identify by its opacity (unlike translucent carnelian), smooth conchoidal fracture, and inability to be scratched by a steel knife. Commonly found in riverbeds and desert environments in the western USA, India, Russia, and Brazil.