
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with Hematite inclusions
AI-generated identification · may be incorrectHardness: 6.5 - 7 on Mohs scale; Color: Opaque brick red to deep orange-red often with white or grey quartz veins; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58 - 2.91
- Hardness
- 6
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5 - 7 on Mohs scale; Color: Opaque brick red to deep orange-red often with white or grey quartz veins; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58 - 2.91
Formation & geological history
Formed through the deposition of silica-rich groundwater into sedimentary or igneous rock cavities. The red color is caused by the inclusion of iron oxide (hematite). It can be found in formations dating back millions of years, often in volcanic ash beds.
Uses & applications
Commonly used in lapidary for jewelry (cabochons, beads), decorative carvings, aquarium gravel, and collected as a 'healing crystal' or metaphysical stone. Historically used for making cylinder seals and ornaments.
Geological facts
Jasper has been a favorite gemstone of the ancient world; it is mentioned in Biblical texts and was used in ancient Mesopotamia to make seals. The name 'Jasper' is derived from the Greek 'iaspis', meaning 'spotted stone'.
Field identification & locations
Identify in the field by its deep red color, opacity (light will not pass through it), and its ability to scratch glass but not be scratched by a steel pocket knife. Found globally, with notable deposits in India, Brazil, Madagascar, and the Southwestern USA.
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