Rock Identifier
Banded Agate (Pink Chalcedony) (Silicon Dioxide (SiO2) - Cryptocrystalline Quartz) — mineral
mineral

Banded Agate (Pink Chalcedony)

Silicon Dioxide (SiO2) - Cryptocrystalline Quartz

Hardness: 6.5-7 on Mohs scale; Color: Pink, white, and translucent lavender bands; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.64

Hardness
6
Color
Pink, white, and translucent lavender bands
Luster
Vitreous to waxy
Identified More mineral

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Physical properties

Hardness: 6.5-7 on Mohs scale; Color: Pink, white, and translucent lavender bands; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.64

Formation & geological history

Formed through the deposition of silica from groundwater in cavities (vesicles) of volcanic igneous rocks or sedimentary formations. The banding occurs due to changes in the chemistry or pressure of the silica-rich fluids over thousands of years.

Uses & applications

Commonly used in the lapidary arts for jewelry (cabochons, beads), decorative ornaments, metaphysical stones, and industrial precision bearings or mortars and pestles due to its hardness.

Geological facts

Agate was named by the Greek philosopher Theophrastus who discovered the stone along the shoreline of the Achates River in Sicily. It has been used for over 3,000 years by ancient civilizations for seal stones and amulets.

Field identification & locations

Identify in the field by its characteristic concentric or parallel banding and toughness; it will scratch glass but cannot be scratched by a steel knife. Common locations include Brazil, Uruguay, Madagascar, and the Lake Superior region of the USA.