
mineral
Banded Agate (specifically Mexican Lace Agate variety appearance)
Silicon Dioxide (SiO2 / Chalcedony)
Hardness: 6.5-7 on Mohs scale. Color: Brown, tan, cream, and grey. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (Trigonal). Cleavage: None (Conchoidal fracture). Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Brown, tan, cream, and grey
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Brown, tan, cream, and grey. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (Trigonal). Cleavage: None (Conchoidal fracture). Specific Gravity: 2.58-2.64.
Formation & geological history
Formed through the deposition of silica from groundwater into cavities (vesicles) in igneous volcanic rocks like rhyolite. The banding results from periodic changes in the chemical composition or temperature of the silica-rich fluids over thousands of years.
Uses & applications
Primarily used for lapidary work including jewelry (cabochons), interior decoration (slabs/bookends), and as metaphysical healing stones. Smaller pieces are often tumbled.
Geological facts
Agates are unique because no two patterns are exactly alike. The term 'agate' is named after the Achates River in Sicily where they were first discovered. Agates have been used by humans for ornaments and tools since Neolithic times.
Field identification & locations
Identify in the field by looking for concentric or wavy banding within a nodule or blocky mass, and its characteristic waxy luster on a fresh break. Common in volcanic regions of Mexico, Brazil, and the Southwestern US. For collectors, look for the 'lace-like' complexity of the bands.
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Mineral
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Mineral/Rock
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