
mineral
Red jasper in gray host rock (likely hematite-stained quartzite or rhyolite)
Jasper: microcrystalline quartz (SiO₂), with iron-oxide coloration; exact host uncertain from image
AI-generated identification · may be incorrectOpaque gray, fine-grained, dull to slightly waxy luster, with irregular brick-red patches likely hematite or red jasper; quartz hardness about 7 Mohs, with no obvious cleavage. Specific gravity is typically about 2.6–2.7.
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Physical properties
Opaque gray, fine-grained, dull to slightly waxy luster, with irregular brick-red patches likely hematite or red jasper; quartz hardness about 7 Mohs, with no obvious cleavage. Specific gravity is typically about 2.6–2.7.
Formation & geological history
Forms when silica-rich fluids replace or cement sediments or volcanic rock, while iron oxides create red coloration; the specimen’s exact geological age and host-rock origin cannot be determined visually.
Uses & applications
Used as lapidary material, cabochons, carvings, tumbled stones, and decorative stone; the rough piece has modest collecting value unless from a distinctive locality.
Geological facts
The red areas may be jasper, hematite, or iron-rich alteration rather than a separate mineral layer. A streak test and hardness testing can distinguish iron oxide from silica-rich jasper.
Field identification & locations
Likely found in iron-rich silica veins, altered volcanic rocks, or sedimentary jasper deposits worldwide. Test an inconspicuous area: quartz-rich material scratches glass, whereas hematite gives a reddish-brown streak and is softer.
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