
sedimentary
Mookaite Jasper
Silicified Radiolarite (SiO2 with impurities)
Hardness: 6.5-7 on Mohs scale; Color: Earth tones like brick red, mustard yellow, cream, and brown; Luster: Vitreous to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7.
- Hardness
- 6
- Color
- Earth tones like brick red, mustard yellow, cream, and brown
- Luster
- Vitreous to dull
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Earth tones like brick red, mustard yellow, cream, and brown; Luster: Vitreous to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7.
Formation & geological history
Formed from the fossilized remains of radiolaria (microscopic marine organisms) whose skeletal remains were deposited in shallow sea beds. Over millions of years (Cretaceous period), these sediments were silicified by groundwater into a porcelain-like chert/jasper.
Uses & applications
Predominantly used as a lapidary material for jewelry (cabochons, beads), decorative carvings, and as a popular specimen for crystal healing and mineral collectors.
Geological facts
Mookaite is found only in one place in the world: the Mooka Creek area in the Kennedy Ranges of Western Australia. The name 'Mooka' is an Aboriginal word meaning 'running waters'.
Field identification & locations
Identify in the field by its distinct 'painterly' bands of yellow and red and its smooth, porcelain-like texture. It occurs as nodules or beds in weathered radiolarite. Collectors should look for vibrant, contrasting color patterns.
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