
mineral
Botryoidal Chalcedony (likely Chert or Agatized Coral)
Silicon Dioxide (SiO2)
Hardness: 6.5-7 on Mohs scale. Color: Waxy tan, white, and earthy brown. Luster: Waxy to vitreous. Crystal Structure: Hexagonal (microcrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.65.
- Hardness
- 6
- Color
- Waxy tan, white, and earthy brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Waxy tan, white, and earthy brown. Luster: Waxy to vitreous. Crystal Structure: Hexagonal (microcrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.65.
Formation & geological history
Formed through the precipitation of silica from groundwater in cavities of volcanic or sedimentary rocks. The 'bubbly' botryoidal texture occurs when minerals grow around a central nucleus. Often found in limestone beds as nodular inclusions.
Uses & applications
Used in lapidary work for making cabochons or beads, landscaping, and as decorative display specimens for mineral collectors.
Geological facts
The term 'botryoidal' comes from the Greek word 'botrys', meaning a bunch of grapes. This specimen appears to have a thick weathering rind (cortex) typical of flint or chert nodules found in the Southeastern United States.
Field identification & locations
Identify in the field by its waxy texture, heavy weight for its size, and the characteristic rounded 'bubbly' surface. It will often scratch glass but cannot be scratched by a steel knife. Common in regions with ancient limestone karst topography.
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