
sedimentary
Weathered chert or silicified limestone nodule
Microcrystalline quartz (SiO₂), possibly replacing limestone; exact identification requires testing
AI-generated identification · may be incorrectCream to tan, dense and fine-grained with a dull-to-waxy luster and irregular solution cavities. Likely hardness about 6.5–7 if chert; limestone would be 3 and fizz strongly with dilute hydrochloric acid. No obvious crystal faces or cleavage are visible.
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Physical properties
Cream to tan, dense and fine-grained with a dull-to-waxy luster and irregular solution cavities. Likely hardness about 6.5–7 if chert; limestone would be 3 and fizz strongly with dilute hydrochloric acid. No obvious crystal faces or cleavage are visible.
Formation & geological history
Probably formed in marine sedimentary rocks as silica-rich material or a silicified limestone concretion, later exposed and rounded by weathering. East Texas near 31.6°N, 95.6°W is dominated by sedimentary formations, making this interpretation regionally plausible; it is not an obvious igneous rock.
Uses & applications
Chert is used historically for sharp tools and occasionally aggregate; limestone is used for cement, lime, roadstone, and construction. This specimen has modest decorative or educational value rather than gemstone value.
Geological facts
The cavities may be weathered fossil, shell, or mineral-remnant spaces. Silicification can preserve textures while replacing the original carbonate.
Field identification & locations
Try a fresh edge: chert can scratch glass, while limestone usually cannot. Apply a drop of vinegar or dilute hydrochloric acid to a concealed spot—vigorous fizz indicates calcite-rich limestone, while no fizz supports chert or silicification. Commonly found as nodules or weathered fragments in regional sedimentary deposits.
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