
sedimentary
Jasper
Silicon Dioxide (SiO2) - Impure Variety of Chert
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Red (due to iron inclusions), brown, yellow; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Red (due to iron inclusions), brown, yellow
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Red (due to iron inclusions), brown, yellow; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.58-2.91
Formation & geological history
Jasper forms when fine silicate materials or volcanic ash are deposited. Over time, heat and pressure transform these into a compact, cryptocrystalline variety of quartz. Red jasper specifically gains its color from the oxidation of iron within the silica during formation.
Uses & applications
Predominantly used as a gemstone for jewelry, lapidary art, and ornamental carvings. Historically used for making tools like scrapers and arrowheads due to its conchoidal fracturing.
Geological facts
In antiquity, Jasper was known as the 'supreme nurturer.' It has been found in archaeological sites dating back to the Neolithic period and was a favorite stone in the ancient world for seals and amulets.
Field identification & locations
Identify in the field by its opaque nature (unlike translucent carnelian), its high hardness (it will scratch glass), and its distinctive smooth, waxy feel. It is commonly found in riverbeds or volcanic regions globally, notably in India, Brazil, and the USA.
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