
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with Hematite impurities
Hardness: 6.5-7 (Mohs scale); Color: Bricky-red to brownish-red; Luster: Vitreous to dull; Crystal Structure: Microcrystalline (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Bricky-red to brownish-red
- Luster
- Vitreous to dull
Identified More sedimentary →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Bricky-red to brownish-red; Luster: Vitreous to dull; Crystal Structure: Microcrystalline (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from hydrothermal solutions or volcanic ash into sedimentary environments. Its red color is derived from iron (hematite) inclusions that occur during the silicification process.
Uses & applications
Predominantly used as a gemstone for jewelry (cabochons, beads), decorative carvings, and in the practice of lapidary arts. Historically used for making tools due to its hardness and fracture pattern.
Geological facts
Jasper was a favorite gem in antiquity and is mentioned in many ancient scriptures and myths. It is known as the 'Supreme Nurturer' in metaphysical circles. In geological terms, it is an opaque variety of chalcedony.
Field identification & locations
Identify in the field by its deep red color, total opacity (it does not transmit light even at the edges), and smooth, waxy feel when water-worn. Common locations include India, Brazil, Egypt, and the Southwestern United States.
More like this
Other sedimentary specimens
Sandstone or Siltstone
Arenite (if sandstone)
Sedimentary
Sandstone
Arenite (primarily SiO2)
sedimentary
Shale or Slaty Mudstone
Argillaceous sedimentary rock
sedimentary
Chert Breccia
Brecciated Chert (Microcrystalline Silica)
sedimentary
Sandstone (Quartz-rich)
Arenite (SiO2)
sedimentary
Sandstone (with man-made markings)
Arenite (composed primarily of Quartz, SiO2)
sedimentary