
sedimentary
Yellow-brown chert or jasper
Microcrystalline quartz (SiO₂), likely iron-oxide-bearing chert/jasper
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; mustard yellow to brown, opaque, waxy-to-dull luster, very fine-grained cryptocrystalline quartz, and conchoidal fracture. Dark veins and gray-white margins may represent iron/manganese oxides and weathered host material.
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Physical properties
Hardness about 6.5–7 Mohs; mustard yellow to brown, opaque, waxy-to-dull luster, very fine-grained cryptocrystalline quartz, and conchoidal fracture. Dark veins and gray-white margins may represent iron/manganese oxides and weathered host material.
Formation & geological history
Forms when silica-rich fluids replace or cement fine sediment, commonly as nodules or beds; coloration comes mainly from iron oxides. The specimen’s precise geological age cannot be determined from the image and depends on its host formation.
Uses & applications
Used as decorative stone, cabochons, beads, carvings, and occasionally aggregate; attractive pieces have modest lapidary value.
Geological facts
Jasper is technically an opaque, impure variety of chert. Its smooth curved fractures and lack of visible crystals help distinguish it from most crystalline igneous rocks.
Field identification & locations
Test for glass-scratching hardness and inspect a fresh fracture for a smooth, waxy surface; avoid relying on color alone. Common worldwide, especially in sedimentary and volcanic terrains.
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