
sedimentary
Snakeskin Jasper
Microcrystalline Quartz (SiO2) with iron inclusions
Hardness: 6.5-7 (Mohs); Color: Gray, tan, and reddish-brown with scale-like patterns; Luster: Vitreous to waxy (when polished); Structure: Trigonal (microcrystalline); Cleavage: None.
- Hardness
- 6
- Color
- Gray, tan, and reddish-brown with scale-like patterns
- Luster
- Vitreous to waxy (when polished)
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Gray, tan, and reddish-brown with scale-like patterns; Luster: Vitreous to waxy (when polished); Structure: Trigonal (microcrystalline); Cleavage: None.
Formation & geological history
Formed primarily in Western Australia as a sedimentary rock where silica-rich fluids permeated older rock layers, depositing microcrystalline quartz in distinct, scale-like bands over millions of years.
Uses & applications
Used extensively in jewelry as cabochons, beads, and pendants, and as a decorative stone for carving and collection.
Geological facts
The 'snakeskin' pattern is a result of chemical processes during formation that create a distinctive texture reminiscent of reptilian scales rather than actual fossilized skin.
Field identification & locations
Identify by the unique rounded, interlocking 'scale' patterns and high hardness; it is commonly sourced from the Windierilla Station area of Western Australia.
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