Rock Identifier
Polished agate nodule (Agate, microcrystalline quartz (SiO₂), likely with chalcedony and iron-oxide inclusions) — gemstone
gemstone

Polished agate nodule

Agate, microcrystalline quartz (SiO₂), likely with chalcedony and iron-oxide inclusions

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; translucent cream, gray, and brown banding with a waxy-to-glassy luster. Microcrystalline quartz has no visible cleavage and conchoidal fracture; the specimen appears cut and polished.

Identified More gemstone
Explore Polished agate nodule in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness 6.5–7 Mohs; translucent cream, gray, and brown banding with a waxy-to-glassy luster. Microcrystalline quartz has no visible cleavage and conchoidal fracture; the specimen appears cut and polished.

Formation & geological history

Agate forms when silica-rich groundwater fills cavities in volcanic rock, depositing chalcedony and quartz in layers, commonly during the Cenozoic or older volcanic episodes. Exact locality cannot be determined from the image.

Uses & applications

Used for cabochons, ornaments, bookends, and lapidary collectibles; it has little industrial value in this small polished form.

Geological facts

The rusty brown areas are likely iron oxides such as hematite or goethite, while the pale translucent material is chalcedony. Agate’s concentric or irregular bands record repeated mineral deposition.

Field identification & locations

Identify by hardness, waxy translucency, curved banding, and resistance to scratching by steel; avoid confusing it with dyed glass or resin. Common sources include Brazil, Uruguay, Mexico, India, and the United States.