
sedimentary
Jasper pebble
Jasper (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 on Mohs scale; Color: Reddish-brown common due to iron inclusions; Luster: Dull to vitreous; Crystal Structure: Microcrystalline/Cryptocrystalline (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58–2.91
- Hardness
- 6
- Color
- Reddish-brown common due to iron inclusions
- Luster
- Dull to vitreous
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Reddish-brown common due to iron inclusions; Luster: Dull to vitreous; Crystal Structure: Microcrystalline/Cryptocrystalline (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58–2.91
Formation & geological history
Formed through the deposition of silica from water or within volcanic ash flows. This specimen shows significant river-worn rounding, indicating transport in a high-energy water environment. While jasper can be any age, many deposits are from the Mesozoic or Paleozoic eras.
Uses & applications
Commonly used in lapidary work for cabochons and beads, as well as industrial abrasives or aquarium gravel. Often collected as decorative pocket stones.
Geological facts
Jasper is an opaque variety of chalcedony. In antiquity, red jasper was associated with vitality and used extensively in seals and amulets across Mesopotamia and Egypt.
Field identification & locations
Identify in the field by its opacity (it will not let light through even at thin edges, unlike agate), smooth water-worn surface, and inability to be scratched by a steel knife. Commonly found in stream beds, beaches, and gravel pits.
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