Rock Identifier
Chalcedony/geode fragment (likely agate with druzy quartz) (Microcrystalline quartz, SiO₂, with possible iron-oxide staining and crystalline quartz) — mineral
mineral

Chalcedony/geode fragment (likely agate with druzy quartz)

Microcrystalline quartz, SiO₂, with possible iron-oxide staining and crystalline quartz

AI-generated identification · may be incorrect

Hardness about 6.5–7 Mohs; gray, brown, cream, and rust-orange coloration; waxy to vitreous luster with sparkling crystal surfaces. Quartz is trigonal and has no cleavage, breaking conchoidally; specific gravity is approximately 2.6.

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Physical properties

Hardness about 6.5–7 Mohs; gray, brown, cream, and rust-orange coloration; waxy to vitreous luster with sparkling crystal surfaces. Quartz is trigonal and has no cleavage, breaking conchoidally; specific gravity is approximately 2.6.

Formation & geological history

Likely formed when silica-rich groundwater filled cavities in volcanic rock, depositing chalcedony and later quartz crystals; iron oxides produced the brown-orange colors. The specimen’s exact geological age cannot be determined from the image.

Uses & applications

Used as a decorative and lapidary stone, including cabochons, polished pieces, and specimen displays; ordinary fragments have modest commercial value.

Geological facts

Agate commonly develops concentric banding, while druzy quartz forms a sugar-like coating of tiny crystals. The image may also show weathered host rock or calcite, so exact identification requires hardness and acid tests.

Field identification & locations

Look for translucent chalcedony, curved banding, and quartz sparkle; quartz should scratch glass, while calcite fizzes in dilute hydrochloric acid. Common sources include Brazil, Uruguay, Mexico, India, and the western United States.