
sedimentary
Jasper
Jasper (Silicon Dioxide, SiO2)
Hardness: 6.5–7 on Mohs scale. Color: Opaque dark green with some tan/brown matrix. Luster: Dull to waxy when unpolished. Crystal system: Trigonal (microcrystalline/cryptocrystalline). Specific Gravity: 2.58–2.91. Cleavage: None, exhibits conchoidal fracture.
- Hardness
- 6
- Color
- Opaque dark green with some tan/brown matrix
- Luster
- Dull to waxy when unpolished
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Physical properties
Hardness: 6.5–7 on Mohs scale. Color: Opaque dark green with some tan/brown matrix. Luster: Dull to waxy when unpolished. Crystal system: Trigonal (microcrystalline/cryptocrystalline). Specific Gravity: 2.58–2.91. Cleavage: None, exhibits conchoidal fracture.
Formation & geological history
Formed through the infiltration of silica-rich fluids into volcanic ash or fine-grained sediments. Over time, the silica crystallizes into microcrystalline quartz. Dark green varieties often get their color from iron silicates or chlorite inclusion.
Uses & applications
Used primarily as an ornamental stone, lapidary work (cabs and tumbling), jewelry (beads and pendants), and as a collector's specimen.
Geological facts
Jasper has been used as a gemstone since antiquity; it was known in ancient Mesopotamian, Greek, and Egyptian cultures. Because of its hardness, it was also used by early humans to create various tools and scrapers.
Field identification & locations
Identify in the field by its hardness (will scratch glass and steel), smooth conchoidal fracture, and complete opacity even when held to a thin light. Often found in stream beds or coastal gravels.
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