
sedimentary
Chert / Chalcedony (Agatized)
Silicon dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brown, tan, and gray swirled; Luster: Waxy to dull; Crystal structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture).
- Hardness
- 6
- Color
- Brown, tan, and gray swirled
- Luster
- Waxy to dull
Identified More sedimentary →
Explore Chert / Chalcedony (Agatized) in the encyclopedia →Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 6.5-7 Mohs; Color: Brown, tan, and gray swirled; Luster: Waxy to dull; Crystal structure: Microcrystalline/cryptocrystalline; Cleavage: None (conchoidal fracture).
Formation & geological history
Formed through the precipitation of silica from groundwater or oceanic fluids, often infilling cavities in limestone or replacing organic material. Typically dated back to various geological eras from Paleozoic to Mesozoic.
Uses & applications
Historically used for stone tools (flint); currently used for lapidary work, tumbling, and as decorative gravel.
Geological facts
This specimen appears to be a water-worn nodule. Chert is extremely durable and chemical resistant, which is why it commonly survives as river gravel long after other rocks erode.
Field identification & locations
Identify by its waxy texture, conchoidal (shell-like) fracture patterns, and hardness (it will scratch glass). Commonly found in riverbeds, glacial till, and sedimentary outcrops.
More like this
Other sedimentary specimens
Fossil-bearing concretion, possibly containing a fossil shell or other organic inclusion
Calcareous concretion; exact fossil and host-rock composition are not identifiable from the image
fossil
Fossiliferous Sedimentary Rock
Sedimentary limestone with invertebrate fossil imprint
fossil
Sandstone or Siltstone
Arenite (if sandstone)
Sedimentary
Sandstone
Arenite
sedimentary
Shale
Shale (clastic sedimentary rock)
sedimentary
Shale (or Mudstone/Siltstone)
Sedimentary Mudrock (SiO2, Al2O3 base with clay minerals)
sedimentary