
sedimentary
Green Jasper (Chert)
Silicon Dioxide (SiO2)
Hardness: 6.5 - 7 on Mohs scale; Color: Dull green with iron-oxide inclusions; Luster: Vitreous to waxy; Crystal structure: Microcrystalline/Cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.6 - 2.9.
- Hardness
- 6
- Color
- Dull green with iron-oxide inclusions
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5 - 7 on Mohs scale; Color: Dull green with iron-oxide inclusions; Luster: Vitreous to waxy; Crystal structure: Microcrystalline/Cryptocrystalline (trigonal); Cleavage: None (conchoidal fracture); Specific gravity: 2.6 - 2.9.
Formation & geological history
Formed through the accumulation of silica-rich fluids in volcanic ash or sedimentary beds. The green color is typically caused by the presence of iron (chlorite or silicate) minerals. Most Jasper dates from various geological eras, notably the Mesozoic and Cenozoic.
Uses & applications
Used primarily in lapidary work for cabochons, beads, and decorative carvings. Industrially, it has historically been used for making tools due to its sharp conchoidal fracture.
Geological facts
Jasper was a favorite gemstone in the ancient world; its name can be traced back in Arabic, Persian, Greek, and Latin. Green Jasper specifically was once considered a powerful 'rain-bringer' in medieval folklore.
Field identification & locations
Identify in the field by its opacity (unlike translucent agate), smooth waxy feel, and characteristic shell-like (conchoidal) chips on the edges. Commonly found in riverbeds or coastal areas in regions like Oregon, Idaho, and Madagascar.
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