Rock Identifier
Chert / Flint Nodule (Microcrystalline quartz (SiO2)) — sedimentary
sedimentary

Chert / Flint Nodule

Microcrystalline quartz (SiO2)

Hardness: 7 on Mohs scale. Color: typically gray, brown, black, or white. Luster: waxy to dull. Crystal structure: microcrystalline/cryptocrystalline quartz (chalcedony). Cleavage: none, conchoidal fracture.

Hardness
7 on Mohs scale
Color
typically gray, brown, black, or white
Luster
waxy to dull
Identified More sedimentary
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Physical properties

Hardness: 7 on Mohs scale. Color: typically gray, brown, black, or white. Luster: waxy to dull. Crystal structure: microcrystalline/cryptocrystalline quartz (chalcedony). Cleavage: none, conchoidal fracture.

Formation & geological history

Formed through the replacement of calcium carbonate by silica-rich solutions in marine environments (such as chalk or limestone beds) over millions of years.

Uses & applications

Historically used for making stone tools, arrowheads, and fire-starting (flint and steel). Modern uses include abrasives and road aggregates.

Geological facts

Chert and flint are chemically identical; the term 'flint' is often used for darker varieties found in chalk formations, while 'chert' refers to varieties found in limestone.

Field identification & locations

Identified by its hard conchoidal fracture and waxy luster. Common in sedimentary rock formations worldwide, particularly chalk and limestone deposits.