
sedimentary
Chert (Jasper variation)
Silicon Dioxide (SiO2) - Microcrystalline Quartz
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Dark brown/black with yellow-brown (ochre) banding, Luster: Waxy to dull, Crystal Structure: Trigonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.7
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Physical properties
Hardness: 7 (Mohs scale), Color: Dark brown/black with yellow-brown (ochre) banding, Luster: Waxy to dull, Crystal Structure: Trigonal (microcrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms) or by the replacement of limestone. This specimen appears to have undergone secondary oxidation or staining, creating the yellow band. Geologically, it can range from Paleozoic to more recent ages.
Uses & applications
Historically used for stone tools due to its sharp conchoidal fracture. Modern uses include decorative lapidary work, jewelry (especially the jasper variety), and as a minor fluxing agent in metallurgical processes.
Geological facts
Chert comes in many varieties; when it is colorful and opaque, it is often called Jasper. It was one of the first minerals utilized by early humans to create arrowheads, knives, and scrapers because of its extreme toughness and sharp edges.
Field identification & locations
Identify in the field by its hardness (it will scratch glass easily), its smooth waxy surface, and characteristic curved (conchoidal) fractures. Commonly found in limestone beds or as stream pebbles.
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