Chert breccia

Hardness: 7 (Mohs scale), Color: Variegated grays, browns, and whites, Luster: Waxy to dull, Crystal structure: Trigonal (microcrystalline/cryptocrystalline), Cleavage: None (conchoidal fracture), Specific gravity: 2.6-2.7

Formed through the mechanical fracturing of chert or flint beds, often due to tectonic movement, karst collapse, or faulting, followed by the cementation of the angular fragments by a silica or carbonate matrix. They are found in many geological eras from Paleozoic to Mesozoic.

Primarily used as decorative stone, aquarium gravel, or historical edge-tool material. In construction, it can be used as fill or road base, though its sharpness and hardness make it less ideal for some concrete aggregates.

Breccia comes from the Italian word for 'loose gravel.' Chert breccias are often indicators of ancient fault zones or sinkhole collapses that happened millions of years ago.

Identify by looking for sharp, angular fragments (clasts) cemented together in a solid matrix. Unlike conglomerate rocks, which have rounded pebbles, breccia fragments maintain their sharp edges. It will scratch glass easily. Common in areas with limestone or ancient seabed deposits.