Blue Agate (Dyed Chalcedony)
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 6.5–7 (Mohs scale); Color: Artificial vibrant blue with white bands; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.64.
Formation & Geological History
Formed as a secondary mineral in cavities within volcanic or metamorphic rocks (vesicles). Silica-rich groundwater deposits layers of microscopically crystalline quartz over long periods. While natural blue agate exists (Blue Lace Agate), this specimen's neon hue is produced through modern chemical dyeing processes.
Uses & Applications
Primarily used for decorative purposes, lapidary workshops, jewelry (pendants and beads), and as a popular item for starting crystal collections.
Geological Facts
Naturally occurring agate is porous, which makes it the most commonly dyed gemstone in history. The practice of coloring agates dates back over 2,000 years to the Romans, who used honey treatments followed by sulfuric acid.
Field Identification & Locations
Identify in the field by its characteristic banding and waxy appearance. Naturally occurring agates are usually duller; vibrant blue specimens like this are almost certainly dyed. Commonly found in Brazil, India, and Madagascar.
Identified on: 4/18/2026
Mode: Standard