
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with iron oxide inclusions
Hardness (Mohs): 6.5-7; Color: Rusty red to brownish-red; Luster: Dull to waxy; Crystal Structure: Microcrystalline/Cryptocrystalline (Hexagonal/Trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Color
- Rusty red to brownish-red
- Luster
- Dull to waxy
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Physical properties
Hardness (Mohs): 6.5-7; Color: Rusty red to brownish-red; Luster: Dull to waxy; Crystal Structure: Microcrystalline/Cryptocrystalline (Hexagonal/Trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the infiltration of silica-rich fluids into volcanic ash or fine-grained sediments, then hardened under pressure. Its red color is derived from high iron content. It can be found in sedimentary beds or as stream/beach pebbles.
Uses & applications
Used primarily as a gemstone for jewelry (cabochons, beads), decorative carvings, and as a popular lapidary material for rock tumbling and polishing.
Geological facts
Jasper was a favorite gem in the ancient world; its name can be traced back in Arabic, Persian, Greek, and Latin. It is often referred to as a 'stone of endurance' in metaphysical circles.
Field identification & locations
Identify in the field by its deep red color, opacity (it does not transmit light even on thin edges), and its ability to scratch glass. Commonly found in riverbeds and on beaches as water-worn pebbles.
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