
mineral
Jasper
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Red, orangish-brown, or reddish-pink; Luster: Dull to waxy; Crystal Structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Red, orangish-brown, or reddish-pink
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Red, orangish-brown, or reddish-pink; Luster: Dull to waxy; Crystal Structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the accumulation of silica-rich fluids in volcanic rocks, sedimentary environments, or as a replacement in hydrothermal processes. Often associated with Cretaceous-age formations in Central Texas (the reported coordinate region), where it is frequently found as river-worn nodules.
Uses & applications
Popular for lapidary work, jewelry (cabochons), river rock landscaping, and as a semi-precious collector's stone. Historically used for making tools due to its conchoidal fracture.
Geological facts
Jasper is an opaque variety of chalcedony. The red color is typically caused by iron inclusions (hematite). It has been used for thousands of years throughout human history for seals and ornaments.
Field identification & locations
Identify in the field by its opacity (unlike translucent agate), its hardness (it will scratch glass), and its smooth, waxy surface when wet. Common in gravel beds and riverbanks across Central and East Texas.
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Sandstone (with potential mineral staining/concretions)
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
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Septarian Pebble
Septarian nodule / Concretion
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