
Mineral variant
Botryoidal Chalcedony (Desert Rose / Agate)
Silicon Dioxide (SiO₂)
Hardness: 6.5-7 (Mohs scale); Color: Gray, blue-gray, black, or tan; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (Microcrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Gray, blue-gray, black, or tan
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Gray, blue-gray, black, or tan; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (Microcrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.58-2.64.
Formation & geological history
Formed through the deposition of silica-rich groundwater in cavities of volcanic or sedimentary rocks. The 'bubbly' botryoidal texture occurs as the mineral grows around a central nucleus, often during the Cenozoic era or more recent geological periods in arid environments.
Uses & applications
Used primarily by rock collectors, in lapidary work for cabochons or beads, and as decorative landscape stones. High-quality specimens are used in metaphysical circles and ornamental jewelry.
Geological facts
The term 'botryoidal' is derived from the Greek word 'botrys,' meaning a bunch of grapes. These specimens are often found in desert regions where volcanic activity once provided the silica and thermal fluids necessary for formation.
Field identification & locations
Identify in the field by looking for rounded, grape-like clusters on the surface of a rock that is too hard to be scratched by a steel knife. Commonly found in the American Southwest (Arizona, Nevada), Mexico, and Morocco. Look for 'vugs' or pockets inside weathered volcanic host rock.
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