
sedimentary
Agate
Silicon Dioxide (SiO2)
Hardness: 6.5-7 (Mohs scale); Color: Banded shades of tan, white, brown, and red; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (Microcrystalline Quartz); Translucent to opaque.
- Hardness
- 6
- Color
- Banded shades of tan, white, brown, and red
- Luster
- Waxy to vitreous
Identified More sedimentary →
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Banded shades of tan, white, brown, and red; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (Microcrystalline Quartz); Translucent to opaque.
Formation & geological history
Formed primarily in volcanic rock cavities (vugs) or certain sedimentary formations by the deposition of silica from groundwater. The bands represent different stages of mineral deposition over thousands of years.
Uses & applications
Used widely in lapidary arts for jewelry, as ornamental stones, in precision pendulums, and historically for mortars and pestles due to its hardness.
Geological facts
Agate is named after the Achates River in Sicily where it was first discovered. No two agates are exactly alike, making each specimen unique. This specific specimen appears to be a water-worn river pebble.
Field identification & locations
Identify by its waxy luster, variety of colors, and characteristic concentric or moss-like banding. Common in riverbeds, gravel pits, and ancient volcanic regions worldwide.
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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Sandstone Grain
Clastic Sedimentary Rock Grain (SiO2 dominated)
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Shale or Slaty Mudstone
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Sandstone
Arenite (primarily SiO2)
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