Rock Identifier
Botryoidal Chalcedony (Agate) (Silicon Dioxide (SiO2)) — mineral
mineral

Botryoidal Chalcedony (Agate)

Silicon Dioxide (SiO2)

Hardness: 6.5-7 Mohs, Color: Yellowish-brown to tan, Luster: Waxy to dull, Crystal Structure: Trigonal (microcrystalline), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.6

Hardness
6
Identified More mineral

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Physical properties

Hardness: 6.5-7 Mohs, Color: Yellowish-brown to tan, Luster: Waxy to dull, Crystal Structure: Trigonal (microcrystalline), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.6

Formation & geological history

Formed primarily by the deposition of silica from groundwater in cavities of volcanic rocks or sedimentary environments. The botryoidal (grape-like) texture occurs when crystals grow around a central nucleus at a uniform rate.

Uses & applications

Used frequently in lapidary work for making cabochons, as a collector's specimen, and historically for making tools due to its hardness and fracture pattern.

Geological facts

The term 'botryoidal' is derived from the Greek word 'botrys', meaning 'bundle of grapes'. Chalcedony is a cryptocrystalline form of silica, meaning its crystals are too small to be seen with a standard microscope.

Field identification & locations

Identify in the field by its distinctive 'bumpy' or mounded surface texture, waxy feel, and extreme hardness (will scratch glass). Commonly found in desert regions, riverbeds, and volcanic ash deposits.