Rock Identifier
Tumbled agate (likely moss or dendritic agate) (Microcrystalline quartz, chiefly chalcedony (SiO₂), with iron-oxide and possible manganese inclusions) — mineral
mineral

Tumbled agate (likely moss or dendritic agate)

Microcrystalline quartz, chiefly chalcedony (SiO₂), with iron-oxide and possible manganese inclusions

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; brown, amber, gray, and translucent; vitreous to waxy luster; cryptocrystalline quartz with no cleavage and conchoidal fracture. Rounded and polished, it appears naturally banded or inclusion-rich.

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Physical properties

Hardness 6.5–7 Mohs; brown, amber, gray, and translucent; vitreous to waxy luster; cryptocrystalline quartz with no cleavage and conchoidal fracture. Rounded and polished, it appears naturally banded or inclusion-rich.

Formation & geological history

Agate forms when silica-rich groundwater fills cavities in volcanic rock, depositing chalcedony and quartz in layers over millions of years, commonly during the Cenozoic or older volcanic episodes.

Uses & applications

Used for cabochons, beads, carvings, bookends, and ornamental objects; valued mainly as an inexpensive collectible gemstone.

Geological facts

The visible pale branching or cloudy patterns may be dendritic inclusions rather than true moss structures; polishing enhances its translucency and color.

Field identification & locations

Identify by its waxy translucence, hardness, conchoidal fracture, and fine banding or mineral inclusions; common sources include Brazil, Uruguay, India, Mexico, Madagascar, and the United States.