
sedimentary
Jasper Beach Pebble
Silicon Dioxide (SiO2) - Macro-crystalline Quartz
AI-generated identification · may be incorrectHardness: 6.5–7 on Mohs scale; Color: Brownish-yellow, tan, and ocher; Luster: Dull to waxy; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58–2.91
- Hardness
- 6
- Color
- Brownish-yellow, tan, and ocher
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Brownish-yellow, tan, and ocher; Luster: Dull to waxy; Crystal Structure: Trigonal/Microcrystalline; 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 during the cooling of the earth's crust. It takes on its rounded, smooth shape through river or ocean wave erosion over thousands of years.
Uses & applications
Used in the lapidary arts for making cabochons and tumbled stones; also common in landscaping, aquarium decor, and pocket stones for meditation or collecting.
Geological facts
Jasper is an impure variety of silica. The name comes from the Old French 'jaspre', meaning 'spotted or speckled stone'. It is distinguished from chalcedony by its opacity, caused by mineral inclusions like iron or clay.
Field identification & locations
Identify in the field by its smooth, water-worn texture and opaque appearance (light does not pass through it). Often found on gravel beaches or in dry riverbeds; this specimen shows characteristic concentric banding or weathering patterns.
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