Rock Identifier
Botryoidal Chalcedony (Chalcedony (SiO2)) — Mineral
Mineral

Botryoidal Chalcedony

Chalcedony (SiO2)

Hardness: 6.5-7 (Mohs scale), Color: Varies widely, but commonly gray, white, blue, brown; can be translucent to opaque. Luster: Waxy to vitreous. Crystal Structure: Cryptocrystalline, meaning the crystals are too fine to be seen without high magnification. Forms in botryoidal (grape-like) aggregates, as seen here.…

Hardness
6
Color
Varies widely, but commonly gray, white, blue, brown
Luster
Waxy to vitreous
Identified More mineral

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Physical properties

Hardness: 6.5-7 (Mohs scale), Color: Varies widely, but commonly gray, white, blue, brown; can be translucent to opaque. Luster: Waxy to vitreous. Crystal Structure: Cryptocrystalline, meaning the crystals are too fine to be seen without high magnification. Forms in botryoidal (grape-like) aggregates, as seen here. No cleavage. Specific Gravity: 2.58-2.64.

Formation & geological history

Chalcedony is a cryptocrystalline variety of quartz. It forms from silica-rich solutions that precipitate in cavities or fissures in rocks. The botryoidal (mammillary) habit results from successive layers of mineral growing outwards from multiple centers on a substrate, creating rounded, grape-like clusters. It can form in various geological environments, including volcanic rocks (like in geodes), sedimentary deposits, and hydrothermal veins. Its geological age varies depending on the specific deposit, ranging from recent to very ancient.

Uses & applications

Used extensively in jewelry as cabochons, beads, and carvings due to its attractive colors and durability. Historically, it was used for tools and arrowheads. Industrially, its hardness and resistance to chemical weathering make it suitable for some specialized applications. The botryoidal form is particularly prized by mineral collectors for its aesthetic appeal.

Geological facts

Many familiar gemstones are varieties of chalcedony, including agate (banded), onyx (parallel bands), jasper (opaque, typically red, yellow, brown, or green), carnelian (red-orange), chrysoprase (apple-green), and bloodstone (dark green with red spots). The botryoidal formation is a secondary mineralization, often occurring in voids left by volcanic activity or dissolution of other minerals.

Field identification & locations

In the field, botryoidal chalcedony is identified by its characteristic rounded, 'grape-like' or 'bubble-like' clusters, waxy luster, and relatively good hardness. Its color can be diverse. It's commonly found in geodes, veins, and cavities in igneous and sedimentary rocks worldwide. Notable localities include Indonesia (for 'grape agate'), Brazil, Uruguay, and various locations in the United States (e.g., Oregon, Arizona). Collectors look for well-formed botryoidal habits and vibrant colors.