
mineral
Agate (Carnelian / Fire Agate nodule)
Silicon Dioxide (SiO2) - Microcrystalline Quartz
Hardness: 6.5-7 on Mohs scale; Color: translucent chalcedony matrix with fiery orange, red-brown, and brownish iron oxide inclusions/botryoidal patterns; Luster: waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture).
- Hardness
- 6
- Luster
- waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: translucent chalcedony matrix with fiery orange, red-brown, and brownish iron oxide inclusions/botryoidal patterns; Luster: waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture).
Formation & geological history
Formed in cavities of volcanic rocks (basalt/andesite) where silica-rich hydrothermal fluids deposited layers of chalcedony over extended periods, often trapped with iron oxides.
Uses & applications
Highly valued as a lapidary material for slicing, polishing, cabochons, jewelry making, and ornamental decorative specimens.
Geological facts
The distinctive orange and red coloration comes from hematite or goethite inclusions trapped inside the translucent chalcedony matrix.
Field identification & locations
Identified by its waxy texture, translucency when backlit, hardness (scratches glass), and characteristic banded or orbicular/botryoidal internal inclusions. Commonly found in gravel beds and volcanic terranes worldwide.
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