
sedimentary
Green Jasper
Silicon Dioxide (SiO2) with iron silicate inclusions
AI-generated identification · may be incorrectHardness: 6.5-7 on the Mohs scale; Color: olive green to deep forest green with dark veining; Luster: waxy to vitreous when wet; Crystal structure: microcrystalline/cryptocrystalline aggregate; Cleavage: none, conchoidal fracture
- Hardness
- 6
- Color
- olive green to deep forest green with dark veining
- Luster
- waxy to vitreous when wet
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Physical properties
Hardness: 6.5-7 on the Mohs scale; Color: olive green to deep forest green with dark veining; Luster: waxy to vitreous when wet; Crystal structure: microcrystalline/cryptocrystalline aggregate; Cleavage: none, conchoidal fracture
Formation & geological history
Formed through the deposition of silica from hydrothermal solutions or sedimentary processes, where iron silicates (like chlorite or actinolite) impart the green coloration. Common in oceanic crust subduction zone mélanges and beach pebble deposits.
Uses & applications
Used widely for lapidary work, cabochons, carved ornaments, tumbled stones, decorative accents, and jewelry making.
Geological facts
Green jasper was highly prized in ancient times and was mentioned in historical texts as a powerful protective stone. It is a dense, opaque variety of chalcedony.
Field identification & locations
Identified in the field by its characteristic smooth, waxy feel when worn by water, distinct conchoidal fracture, hardness (scratches glass), opaque nature, and dull to waxy luster. Commonly found along beaches and riverbeds in coastal regions, particularly in California and Oregon.
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