
sedimentary
Jasper Pebble (Quartzite / Chert)
Microcrystalline Quartz (SiO2 with iron oxide inclusions)
AI-generated identification · may be incorrectHardness: 6.5 - 7 on Mohs scale; Color: Reddish-brown, tan, and mottled cream; Luster: Waxy to dull; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58 - 2.91
- Hardness
- 6
- Color
- Reddish-brown, tan, and mottled cream
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5 - 7 on Mohs scale; Color: Reddish-brown, tan, and mottled cream; Luster: Waxy to dull; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58 - 2.91
Formation & geological history
Formed through the deposition of silica-rich fluids within sedimentary or volcanic host rocks, frequently colored by iron oxides. This rounded specimen was further shaped and smoothed by fluvial or coastal water erosion.
Uses & applications
Commonly collected as decorative garden stones, tumbled for lapidary work, cabochons, and beginner jewelry crafting.
Geological facts
Jasper has been used by ancient humans for thousands of years both for carving amulets and ornaments, as well as for knapping into sharp stone tools due to its conchoidal fracture.
Field identification & locations
Identify in the field by its hardness (scratches glass easily, cannot be scratched by a steel nail), smooth water-worn surface, and reddish-tan jasperoid hue. Frequently discovered along river gravels, creek beds, and beaches worldwide.
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