
sedimentary
Jasper containing fossilized inclusions
Silicon Dioxide (SiO2) with trace impurities and biogenic inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Dark brown to mottled earth tones with lighter fossil centers, Luster: Vitreous to dull, Crystal structure: Microcrystalline/Cryptocrystalline, No cleavage, Specific gravity: 2.6-2.9
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Dark brown to mottled earth tones with lighter fossil centers, Luster: Vitreous to dull, Crystal structure: Microcrystalline/Cryptocrystalline, No cleavage, Specific gravity: 2.6-2.9
Formation & geological history
Formed through the silicification of fine-grained sediment or organic matter. Over millions of years (often Mesozoic or Cenozoic), silica-rich water permeates the sediment, replacing organic structures with quartz/chalcedony. This specific piece appears to be a stream-tumbled pebble.
Uses & applications
Commonly used for lapidary work (cabochons), jewelry making, landscape stone, and as a decorative collector's item due to its unique patterns.
Geological facts
Jasper is an opaque variety of chalcedony. When it contains visible fossils like shells, coral, or crinoids, it is often nicknamed 'Fossil Jasper.' The circular white/grey inclusion in the center appears to be a small cross-section of a fossilized aquatic organism.
Field identification & locations
Identify in the field by its hardness (will scratch glass), smooth waxy texture when wet, and the presence of intricate or circular 'eyes' which are fossil cross-sections. Commonly found in riverbeds and gravel deposits worldwide.
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