
sedimentary
Red Jasper
Silicon Dioxide (SiO2) with Hematite impurities
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Brick red to deep terracotta; Luster: Vitreous to dull/waxy when polished; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Brick red to deep terracotta
- Luster
- Vitreous to dull/waxy when polished
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Brick red to deep terracotta; Luster: Vitreous to dull/waxy when polished; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed through the deposition of silica from mineral springs or hydrothermal vents into volcanic or sedimentary rocks. The red coloring comes from high iron/hematite content. It can be found in formations ranging from Precambrian to recent ages.
Uses & applications
Mostly used for semi-precious jewelry (beads, cabochons), ornamental carvings, stone inlays, and as a popular stone for gemstone collecting and lapidary practice.
Geological facts
Jasper has been used as a gemstone since antiquity; it was known as the 'rain bringer' in some Native American cultures and was featured in the breastplate of the High Priest in Biblical descriptions.
Field identification & locations
Identify in the field by its opaque nature (unlike Carnelian which is translucent), its smooth waxy surface when damp, and its extreme hardness (will scratch glass). Commonly found in riverbeds and coastal regions of South Africa, Brazil, and the Southwestern USA.
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