
mineral
Agate Geode Slice (with Druzy Quartz)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Grayish-blue outer chalcedony with a yellowish-white crystalline center; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (agate) with macrocrystalline quartz in the center; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.65
- Hardness
- 6
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Grayish-blue outer chalcedony with a yellowish-white crystalline center; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (agate) with macrocrystalline quartz in the center; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.65
Formation & geological history
Formed as secondary deposits in volcanic rock cavities (vesicles) or sedimentary pockets. Siliceous groundwater permeates the rock, slowly depositing layers of chalcedony over thousands of years. The central opening indicates it is part of a geode where crystals had space to grow inward.
Uses & applications
Primarily used for decorative purposes, gemstone collecting, metaphysical jewelry, and lapidary art.
Geological facts
Agate is named after the Achates River in Sicily. The concentric banding visible in such specimens is actually rhythmic layers of silica and impurities. The small, sparkling crystals in the center are known as 'druzy' quartz.
Field identification & locations
Identify in the field by looking for rounded, lumpy nodules with a rough, dull exterior that feels heavy for its size. High-quality pieces are typically sourced from Brazil, Uruguay, and Oregon, USA. This specific shape is a custom-cut and polished slab designed for display.
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