Rock Identifier
Polished agate geode (Microcrystalline quartz (chalcedony), SiO₂, with possible druzy quartz and iron-oxide inclusions) — mineral
mineral

Polished agate geode

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

AI-generated identification · may be incorrect

Hardness 6.5–7 Mohs; cream, tan, gray, and brown concentric banding; waxy to vitreous luster; cryptocrystalline quartz with cavities lined by small crystals. Agate has no visible cleavage and typically has specific gravity around 2.6.

Identified More mineral
Explore Polished agate geode in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness 6.5–7 Mohs; cream, tan, gray, and brown concentric banding; waxy to vitreous luster; cryptocrystalline quartz with cavities lined by small crystals. Agate has no visible cleavage and typically has specific gravity around 2.6.

Formation & geological history

Silica-rich groundwater filled vesicles or cavities in volcanic rock, depositing chalcedony in successive bands and later quartz crystals in open voids. The specimen is likely Cenozoic or older, but its exact age cannot be determined from the image.

Uses & applications

Used as a decorative polished specimen, cabochon, carving material, and occasionally in jewelry; agate is also used for beads, bookends, and ornamental objects.

Geological facts

The rounded cavities and layered, flowing bands are characteristic of botryoidal or fortification agate. Dark interiors may contain druzy quartz or iron/manganese staining.

Field identification & locations

Identify by its translucent waxy banding, conchoidal fracture, and hardness sufficient to scratch glass; a steel blade should not easily scratch it. Common sources include Brazil, Uruguay, Mexico, India, Madagascar, and the western United States.