
mineral
Dendritic Agate (Tree Agate)
Chalcedony (Silicon Dioxide, SiO2) with Manganese or Iron Oxide inclusions
Hardness: 6.5-7 (Mohs scale); Color: White, gray, or translucent base with dark branch-like patterns; Luster: Waxy to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.58-2.64
- Hardness
- 6
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: White, gray, or translucent base with dark branch-like patterns; Luster: Waxy to vitreous; Crystal Structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.58-2.64
Formation & geological history
Formed when mineral-rich water (containing manganese or iron) seeps into cracks in chalcedony or limestone. The patterns grow in a fractal manner similar to frost. Most specimens are found in volcanic rocks or alluvial deposits and can be millions of years old.
Uses & applications
Primarily used in jewelry (cabochons), lapidary art, and as a collector's specimen. In industry, high-quality chalcedony can be used as a precision bearing or abrasive.
Geological facts
The term 'dendrite' comes from the Greek word 'dendron' meaning tree. Despite the botanical appearance, these patterns are purely mineral and contain no organic fossil material. They are often mistaken for fossilized moss or ferns.
Field identification & locations
Identify in the field by its characteristic 'fern-like' or 'branch-like' black or brown patterns against a lighter rock matrix. It is commonly found in India, Brazil, and the Western United States. Collectors should look for high contrast and clear patterns.
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