Banded Agate
Silicon Dioxide (SiO2) - variety Chalcedony
Rock Type: mineral

Physical Properties
Hardness: 6.5-7 (Mohs scale); Color: Gray, black, and brown banding; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.64.
Formation & Geological History
Formed in cavities of volcanic rocks or ancient lavas, where silica-rich groundwater deposited layers of microcrystalline quartz over time, often resulting in rhythmic banding.
Uses & Applications
Used primarily in lapidary arts for jewelry (cabochons, beads), decorative ornaments, and as a healing stone in metaphysical communities. Historically used for making precision bearings and mortar and pestle sets.
Geological Facts
The name Agate comes from the Achates River in Sicily, where agates were first discovered by the Greek philosopher Theophrastus around the 4th century BC. Each stone's banding pattern is unique like a fingerprint.
Field Identification & Locations
Identify in the field by its distinct translucent or opaque banding, lack of cleavage, and extreme hardness (will scratch glass). Commonly found in riverbeds, shorelines, and areas with ancient volcanic activity.
Identified on: 4/15/2026
Mode: Standard