
sedimentary
River Jasper
Silicon Dioxide (SiO2) with impurities
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Olive green to yellow-tan with brownish iron-oxide veining; Luster: Waxy to dull (wet appearance is vitreous); Structure: Microcrystalline quartz; Cleavage: None (Conchoidal fracture).
- Hardness
- 6
- Color
- Olive green to yellow-tan with brownish iron-oxide veining
- Luster
- Waxy to dull (wet appearance is vitreous)
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Physical properties
Hardness: 6.5-7 Mohs; Color: Olive green to yellow-tan with brownish iron-oxide veining; Luster: Waxy to dull (wet appearance is vitreous); Structure: Microcrystalline quartz; Cleavage: None (Conchoidal fracture).
Formation & geological history
Formed primarily in sedimentary environments where silica-rich fluids permeate porous volcanic ash or sedimentary beds. This specific specimen has been water-shaped and smoothed by fluvial (river) erosion over many years.
Uses & applications
Used for lapidary work, tumbled stones, jewelry (cabochons), and as decorative aquarium or landscaping stones.
Geological facts
Jasper is an opaque variety of chalcedony. The veins seen in this specimen are often 'healed' fractures where secondary minerals like iron oxides or manganese have filled in over geological time.
Field identification & locations
Identified in the field by its smooth, river-worn texture, opacity (does not let light through), and high hardness—it will easily scratch glass but cannot be scratched by a steel knife. Common in gravel beds and riverbanks.
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