
mineral
Agate
Cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7; Color: Creamy white to translucent with a reddish-brown matrix; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Specific gravity: 2.58–2.64
- Hardness
- 6
- Color
- Creamy white to translucent with a reddish-brown matrix
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5–7; Color: Creamy white to translucent with a reddish-brown matrix; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Specific gravity: 2.58–2.64
Formation & geological history
Formed as secondary deposits in cavities (vesicles) within igneous volcanic rocks, such as basalt. Silica-rich groundwater permeates these pockets, depositing layers of chalcedony over thousands to millions of years.
Uses & applications
Used primarily in lapidary arts for jewelry, bead making, and ornamental carvings. Historically used for making mortars and pestles due to its hardness.
Geological facts
The specimen shown appears to be a whole or split agate nodule, often called a 'Thunder Egg' depending on its locality. Agates are named after the Achates River in Sicily where they were first discovered.
Field identification & locations
Identify in the field by looking for a waxy luster on broken surfaces, a translucent quality when held to light, and an often rough, bumpy exterior 'skin' that hides the interior crystal or band structure. Common in the Pacific Northwest and volcanic regions.
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