
sedimentary
Geodal Limestone / Calcite Druze
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: Tan, beige, to off-white; Luster: Vitreous to pearly crystals on a dull earthy matrix; Crystal Structure: Trigonal/Rhombohedral; Cleavage: Perfect rhombohedral in crystal areas; Specific Gravity: 2.71
- Hardness
- 3 on Mohs scale
- Color
- Tan, beige, to off-white
- Luster
- Vitreous to pearly crystals on a dull earthy matrix
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Physical properties
Hardness: 3 on Mohs scale; Color: Tan, beige, to off-white; Luster: Vitreous to pearly crystals on a dull earthy matrix; Crystal Structure: Trigonal/Rhombohedral; Cleavage: Perfect rhombohedral in crystal areas; Specific Gravity: 2.71
Formation & geological history
Formed through the chemical precipitation of calcium carbonate from groundwater within cavities (vugs) of limestone or dolostone bedrock. These often date from the Paleozoic to Mesozoic eras and form in marine environments or karst landscapes.
Uses & applications
Primarily used as decorative garden stones, aquarium rocks, or entry-level mineral specimens for collectors. Industrial grade limestone is used in cement production and as a soil conditioner.
Geological facts
Vuggy limestone like this specimen often contains 'druze'—tiny sparkling crystal coatings. If a drop of vinegar or weak acid is applied, the specimen will fizz (effervesce) due to the release of carbon dioxide gas.
Field identification & locations
Identify in the field by its relatively soft surface (rank with a copper penny) and the presence of small botryoidal or crystalline clusters in hollows. Commonly found in road cuts or quarries in the Midwest USA and other limestone-rich regions.
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