
sedimentary
Agate (Geode/Nodule)
Chalcedony (cryptocrystalline silica, SiO2)
Hardness: 6.5-7 (Mohs scale), Color: Brown, tan, and grey with possible internal banding, Luster: Waxy to vitreous, Crystal Structure: Trigonal (microscopic), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.60-2.65
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Brown, tan, and grey with possible internal banding, Luster: Waxy to vitreous, Crystal Structure: Trigonal (microscopic), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.60-2.65
Formation & geological history
Formed primarily as nodules in volcanic rocks or certain sedimentary rocks where silica-rich groundwater fills cavities left by gas bubbles or dissolved organic material. Most range from 20 to 100 million years old, depending on the host formation.
Uses & applications
Used extensively in jewelry (cabochons), interior decor, abrasive tools specifically mortar and pestle sets, and as a popular collector's item for lapidary work.
Geological facts
Agate was named by the Greek philosopher Theophrastus who discovered the stone along the shore line of the river Achates in Sicily. No two natural agates are identical in their internal banding patterns.
Field identification & locations
Identified in the field by its characteristic 'orange peel' or bumpy exterior texture and conchoidal (shell-like) fracture edges. Commonly found in riverbeds, desert pavements, and volcanic ash deposits in places like Brazil, Uruguay, and the US Northwest.
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