
sedimentary
Agate (specifically Chalcedony/Banded Agate)
Silicon Dioxide (SiO2)
Hardness: 6.5–7 (Mohs scale); Color: White, translucent, and grayish-blue banding; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.60–2.65
- Hardness
- 6
- Color
- White, translucent, and grayish-blue banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: White, translucent, and grayish-blue banding; Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.60–2.65
Formation & geological history
Formed in cavities (vesicles) of volcanic rocks or sedimentary formations where silica-rich groundwater deposits layers over time. This specimen shows classic botryoidal-style banding indicative of secondary silica deposition.
Uses & applications
Used primarily in lapidary arts for jewelry, ornamental carvings, and as a semi-precious gemstone. Also used historically for precision bearings and mortars/pestles due to its hardness.
Geological facts
Agate is a variety of chalcedony characterized by its fineness of grain and brightness of color. It was named by Theophrastus, a Greek philosopher, who discovered the stone along the shore line of the Dirillo River in Sicily.
Field identification & locations
Identify in the field by its waxy texture, translucency when held to light, and characteristic concentric or parallel banding. This specific piece appears to be a seam agate or a fragment of a larger geode wall.
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