mineral

Agate

Silicon Dioxide (SiO2) - Chalcedony variety

AI-generated identification · may be incorrect

Hardness: 6.5–7 (Mohs); Color: Multi-colored (white, grey, blue-grey in this specimen); Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (Trigonal/Monoclinic); Cleavage: None; Fracture: Conchoidal; Specific Gravity: 2.58–2.64.

Hardness: 6
Color: Multi-colored (white, grey, blue-grey in this specimen)
Luster: Waxy to vitreous

Identified April 19, 2026More mineral →

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Physical properties

Formation & geological history

Formed from silica-rich groundwater filling cavities (vugs) in volcanic or sedimentary rocks. Over time, layers of microcrystalline quartz deposit sequentially, creating a banded appearance. They are often found in Cenozoic or Mesozoic volcanic host rocks.

Uses & applications

Used primarily in lapidary arts, jewelry, decorative carvings, and as a gemstone. Historically used for making mortars and pestles or burnishing tools due to its hardness.

Geological facts

Agate is named after the Achates River (now the Dirillo River) in Sicily. It is unique because no two agates are exactly alike; the banding patterns are a result of fluctuating chemical conditions during formation.

Field identification & locations

Identify in the field by its translucent edges, waxy luster when broken, and characteristic concentric or parallel banding patterns. Look for nodules with a weathered, 'pitted' or 'brain-like' exterior in riverbeds or volcanic ash areas.