Rock Identifier
Polished chalcedony (likely sagenite or included agate) (Microcrystalline quartz, SiO₂, with iron-oxide and possibly rutile/goethite inclusions) — gemstone
gemstone

Polished chalcedony (likely sagenite or included agate)

Microcrystalline quartz, SiO₂, with iron-oxide and possibly rutile/goethite inclusions

AI-generated identification · may be incorrect

A polished, translucent tan-brown sphere with gray-white chalcedony, honey-colored zones, and dark/golden inclusions; vitreous to waxy luster. Mohs hardness 6.5–7, cryptocrystalline quartz structure, no visible cleavage, specific gravity about 2.6.

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Physical properties

A polished, translucent tan-brown sphere with gray-white chalcedony, honey-colored zones, and dark/golden inclusions; vitreous to waxy luster. Mohs hardness 6.5–7, cryptocrystalline quartz structure, no visible cleavage, specific gravity about 2.6.

Formation & geological history

Forms when silica-rich groundwater fills cavities and fractures in volcanic rocks, depositing chalcedony in bands and trapping iron oxides or other minerals; inclusions and color develop during later mineralization. Typically Cenozoic to older volcanic-host-rock age.

Uses & applications

Used as a decorative sphere, lapidary ornament, paperweight, and collectible gemstone; similar included agates are also used in cabochons and jewelry.

Geological facts

The internal patterns are natural mineral inclusions rather than visible quartz crystals. Strong translucency and irregular flow-like banding are characteristic of chalcedony-based agate.

Field identification & locations

Identify by its cool, dense feel, glassy polish, translucency, and resistance to scratching by steel; glass or resin may show bubbles, but testing should be done inconspicuously. Common sources include Brazil, Uruguay, Mexico, Madagascar, and the United States.