
mineral
Agate and Chalcedony Assortment
Silicon Dioxide (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Multi-colored, translucent to semi-transparent; Luster: Vitreous to waxy; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None; Fracture: Conchoidal; Specific Gravity: 2.60-2.65.
- Hardness
- 6
- Color
- Multi-colored, translucent to semi-transparent
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Multi-colored, translucent to semi-transparent; Luster: Vitreous to waxy; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None; Fracture: Conchoidal; Specific Gravity: 2.60-2.65.
Formation & geological history
Formed primarily in volcanic and metamorphic rocks as silica-rich groundwater fills cavities (vesicles). They are cryptocrystalline varieties of quartz, often found in Cenozoic era volcanic deposits.
Uses & applications
Used extensively in jewelry as gemstones (cabochons and beads), ornamental carvings, burnishing tools, and for lapidary precision instruments due to their hardness.
Geological facts
Agates are famous for their distinct banding patterns, caused by rhythmic crystallization of silica layers. The Greek philosopher Theophrastus named the stone after the Achates River in Sicily where it was first discovered.
Field identification & locations
Identify in the field by looking for a waxy luster on fractured surfaces and a lack of visible crystal grains. These tumbled specimens are common in riverbeds and beaches in volcanic regions globally, such as Brazil, India, and the United States (Oregon/Lake Superior).
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral