Rock Identifier
Chalcedony / Agate Nodule (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Chalcedony / Agate Nodule

Silicon Dioxide (SiO2)

Mohs hardness of 6.5 to 7; color ranges from grey, white, to brownish tones; vitreous to waxy luster; cryptocrystalline structure; conchoidal fracture with no true cleavage; specific gravity of 2.58 to 2.64.

Identified More sedimentary
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Physical properties

Mohs hardness of 6.5 to 7; color ranges from grey, white, to brownish tones; vitreous to waxy luster; cryptocrystalline structure; conchoidal fracture with no true cleavage; specific gravity of 2.58 to 2.64.

Formation & geological history

Formed through the deposition of silica-rich groundwater solutions in cavities or fractures of rocks, typically volcanic or sedimentary, over millions of years.

Uses & applications

Used in ornamental carvings, lapidary arts, jewelry, and prized by mineral collectors.

Geological facts

Chalcedony is a cryptocrystalline form of silica, meaning its crystals are too small to be seen without high magnification. Nodules often form hollow cavities lined with tiny quartz or chalcedony crystals, creating mini-geodes.

Field identification & locations

Can be identified in the field by its waxy luster, conchoidal fracture, and resistance to scratching steel. Frequently found in regions with historical volcanic activity or limestone formations containing silica nodules.