
sedimentary
Rounded gray-green chert (likely silicified limestone)
Microcrystalline quartz/chalcedony (SiO₂), possibly jasper or siliceous limestone
AI-generated identification · may be incorrectHardness about 6.5–7 Mohs; pale gray-green with cream and rusty weathering veins, dull to waxy luster, very fine-grained and massive, with no visible cleavage. It appears water-worn and smoothly rounded.
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Physical properties
Hardness about 6.5–7 Mohs; pale gray-green with cream and rusty weathering veins, dull to waxy luster, very fine-grained and massive, with no visible cleavage. It appears water-worn and smoothly rounded.
Formation & geological history
Formed when silica replaced or cemented carbonate sediment, commonly during diagenesis; its exact geological age cannot be determined from the image. Later stream or shoreline transport produced the rounded shape.
Uses & applications
Common chert is used locally as aggregate, road material, landscaping stone, and historically for tools; attractive pieces may be polished as decorative objects. Typical specimens have modest value.
Geological facts
Chert commonly breaks with a curved, conchoidal fracture and can produce sharp edges. Green coloration may reflect chlorite, iron-poor minerals, or other trace impurities.
Field identification & locations
Identify it by its dense, lightweight-for-size feel, waxy surface, lack of visible grains, and ability to scratch ordinary glass; a steel file should leave little mark. Chert occurs widely in sedimentary formations and stream gravels worldwide.
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