
mineral
Dendritic Agate
Silicon Dioxide (SiO2) with Manganese/Iron oxide inclusions
Hardness: 6.5-7 (Mohs scale), Color: Translucent white to gray with black/brown tree-like inclusions, Luster: Vitreous to waxy, Crystal structure: Trigonal/Hexagonal (cryptocrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.58-2.64
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Translucent white to gray with black/brown tree-like inclusions, Luster: Vitreous to waxy, Crystal structure: Trigonal/Hexagonal (cryptocrystalline), Cleavage: None (conchoidal fracture), Specific Gravity: 2.58-2.64
Formation & geological history
Formed through the deposition of silica from groundwater in cavities of igneous rocks. The dendritic patterns are created when manganese or iron oxides seep into cracks and crystallize in branching patterns during or after the agate formation.
Uses & applications
Primarily used in jewelry (cabochons), lapidary art, and as metaphysical or collector specimens. Also historically used for amulets and seals.
Geological facts
Despite the name, dendritic agate is often technically a chalcedony rather than a true agate because it typically lacks the concentric banding characteristic of Agate. The 'tree-like' patterns are purely mineral and are not fossilized plants.
Field identification & locations
Identify by its translucent body and distinctive fern-like or moss-like black/brown inclusions. Found commonly in Brazil, India, Madagascar, and the USA (notably Montana and Oregon). Collectors look for high contrast and clear patterns.
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