
mineral
Agate (Moss or Plume Agate variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale). Color: White, translucent centers with brown, orange, and green inclusions. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (cryptocrystalline). Cleavage: None, conchoidal fracture.
- Hardness
- 6
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale). Color: White, translucent centers with brown, orange, and green inclusions. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (cryptocrystalline). Cleavage: None, conchoidal fracture.
Formation & geological history
Formed through the deposition of silica from groundwater in the cavities of igneous rocks, particularly volcanic lavas. Most are deposited in layers or dendritic patterns over thousands of years.
Uses & applications
Used primarily in lapidary arts, jewelry (cabochons), interior decoration, and as a collector's specimen. Historically used for making mortars and pestles because of its hardness.
Geological facts
Agates are found inside geodes or as nodules in volcanic rock. The unique colors are often caused by trace amounts of iron, manganese, or nickel. Many specimens from the American West date back to the Eocene epoch.
Field identification & locations
Identify in the field by its waxy texture and translucent 'window' when held to light. It lacks the graininess of sandstone and is hard enough to scratch glass. Commonly found in riverbeds or desert regions of the Western US.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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Septarian Pebble
Septarian nodule / Concretion
sedimentary