
sedimentary
Jasper with Manganese Dendrites
Silicon Dioxide (SiO2) with Oxide Mineral Inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: tan, yellow, and brownish background with black/dark grey dendritic patterns; Luster: dull to vitreous; Crystal Structure: Microcrystalline (Trigonal); Cleavage: none (conchoidal fracture); Specific Gravity: 2.58-2.91.
- Hardness
- 6
- Luster
- dull to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs); Color: tan, yellow, and brownish background with black/dark grey dendritic patterns; Luster: dull to vitreous; Crystal Structure: Microcrystalline (Trigonal); Cleavage: none (conchoidal fracture); Specific Gravity: 2.58-2.91.
Formation & geological history
Formed through the accumulation of fine-grained silica-rich sediments or volcanic ash. The dark 'tree-like' patterns are manganese oxides that crystallized from mineral-rich water seeping into tiny cracks or fractures in the stone over millions of years.
Uses & applications
Commonly used as lapidary material for cabochons, beads, and decorative carvings. Larger specimens are valued by rockhounds and mineral collectors as display pieces.
Geological facts
The black patterns are often mistaken for fossilized plants (ferns or moss), but they are actually inorganic crystal growths known as dendrites. The name 'Jasper' is derived from the Greek word 'iaspis', meaning spotted stone.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), its opaque nature, and the distinct branching dark patterns. Found globally, especially in desert regions or areas with high volcanic activity like the Western United States, India, and Australia.
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