Rock Identifier
Botryoidal Quartz / Calcite Geode crust (Silicon Dioxide (SiO2) or Calcium Carbonate (CaCO3)) — mineral
mineral

Botryoidal Quartz / Calcite Geode crust

Silicon Dioxide (SiO2) or Calcium Carbonate (CaCO3)

Hardness: 7 (if quartz) or 3 (if calcite); Color: White, cream, or colorless; Luster: Vitreous to pearly; Crystal structure: Trigonal or Hexagonal; Specific gravity: 2.65 or 2.71

Hardness
7 (if quartz) or 3 (if calcite)
Color
White, cream, or colorless
Luster
Vitreous to pearly
Identified More mineral

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Physical properties

Hardness: 7 (if quartz) or 3 (if calcite); Color: White, cream, or colorless; Luster: Vitreous to pearly; Crystal structure: Trigonal or Hexagonal; Specific gravity: 2.65 or 2.71

Formation & geological history

Formed through hydrothermal precipitation in rock cavities or vugs, where mineral-rich water slowly deposits layers over thousands of years.

Uses & applications

Commonly used for geological displays, decorative home decor, crystal healing collections, and educational specimens.

Geological facts

Botryoidal formations get their name from the Greek word 'botrys', meaning a bunch of grapes, due to the rounded, bubbly appearance of the mineral growth.

Field identification & locations

Identified by its cauliflower-like or 'bubbly' texture. To distinguish between quartz and calcite, one can perform an acid test (calcite fizzes) or a hardness test (quartz scratches glass).