Rock Identifier
Chalcedony or chert pebble with iron-oxide staining (Microcrystalline quartz (SiO₂), possibly a weathered chert or flint nodule) — sedimentary
sedimentary

Chalcedony or chert pebble with iron-oxide staining

Microcrystalline quartz (SiO₂), possibly a weathered chert or flint nodule

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; gray-brown, dull to waxy luster, very fine-grained and conchoidally fracturing. The pale outer rind and darker interior suggest weathering and iron/mineral staining; no visible cleavage.

Identified More sedimentary
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Physical properties

Hardness about 6.5–7 Mohs; gray-brown, dull to waxy luster, very fine-grained and conchoidally fracturing. The pale outer rind and darker interior suggest weathering and iron/mineral staining; no visible cleavage.

Formation & geological history

Likely formed when silica-rich groundwater replaced or cemented sediment, producing microcrystalline quartz; the outer cortex developed during weathering. Exact geological age cannot be determined from the photograph.

Uses & applications

Used historically for cutting tools and fire-starting, and today as a lapidary or collecting material; generally not valuable as construction stone.

Geological facts

Chert and chalcedony are varieties of microcrystalline quartz, often difficult to distinguish visually without testing. The dark center may also represent a silicified fossil or another included mineral.

Field identification & locations

Common in river gravels, limestone terrains, and weathered sedimentary formations. Test with a steel file or glass: genuine quartz-rich chert can scratch glass; a freshly broken surface should be smooth and waxy rather than granular.