Botryoidal Chalcedony
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 6.5-7 (Mohs scale); Color: White, translucent to waxy; Luster: Vitreous to waxy; Crystal structure: Trigonal (cryptocrystalline); Cleavage: None; Specific Gravity: 2.58-2.64
Formation & Geological History
Formed through the precipitation of silica from groundwater in the cavities of volcanic or sedimentary rocks, often in hydrothermal environments.
Uses & Applications
Commonly used as a gemstone for jewelry, in lapidary work for carvings, and as a popular specimen for mineral collectors.
Geological Facts
The term 'botryoidal' comes from the Greek word 'botrys', meaning a bunch of grapes, referring to its rounded, globular external form. Chalcedony is a cryptocrystalline form of silica, meaning its crystals are too small to be seen without high magnification.
Field Identification & Locations
Identified by its 'grape-like' bubbles and waxy surface. It is commonly found in basalt cavities (geodes) or as a replacement mineral in wood and fossils. Collectors look for pieces with high translucency or unique surface patterns.
Identified on: 5/15/2026
Mode: Standard