Rock Identifier
Chert (or potentially massive Quartz/Quartzite) (SiO2 (Silicon Dioxide)) — sedimentary (if chert) / metamorphic (if quartzite)
sedimentary (if chert) / metamorphic (if quartzite)

Chert (or potentially massive Quartz/Quartzite)

SiO2 (Silicon Dioxide)

Hardness: 7 on Mohs scale. Color: Variable, typically tan, brown, gray, or banded. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline or microcrystalline.

Hardness
7 on Mohs scale
Color
Variable, typically tan, brown, gray, or banded
Luster
Waxy to vitreous

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 7 on Mohs scale. Color: Variable, typically tan, brown, gray, or banded. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline or microcrystalline.

Formation & geological history

Formed from silica-rich fluids precipitating in sedimentary rocks, often replacing limestone. Or formed from the metamorphism of sandstone.

Uses & applications

Historically used for making stone tools (arrowheads, scrapers). Currently used occasionally as a low-grade construction aggregate, or polished for lapidary uses if attractively banded.

Geological facts

Chert was a crucial material for early humans to create sparking tools for fire and sharp edges for tools and weapons.

Field identification & locations

Identified by its conchoidal fracture (curved break), high hardness (scratches glass), and waxy luster. Common in many sedimentary terrains worldwide.