
Dolomite is a sedimentary rock composed mainly of the mineral dolomite (calcium magnesium carbonate). It forms from limestone through a process called dolomitization. Dolomite is harder than limestone and is used in construction and as a source of magnesium.
| Texture | Crystalline |
| Colors | White, gray, pink, tan, yellow |
| Magnetism | Non-magnetic |
| Grain Size | Variable |
| Hardness | 3.5-4 |
| Density | 2.8-2.9 g/cm³ |
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Main Elements:
Ca, Mg, C, O
Chemical Composition:
CaMg(CO₃)₂ (Calcium Magnesium Carbonate)
Dolomite dust can cause respiratory irritation. Generally safe to handle, but avoid inhaling dust particles.
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Density:
2.8-2.9 g/cm³
Compressive Strength:
50-250 MPa
Melting Point:
Decomposes at 800-900°C
Formation:
Forms from limestone through dolomitization, where magnesium replaces some calcium in the presence of magnesium-rich water.
Composition:
Composed primarily of the mineral dolomite (CaMg(CO₃)₂), which is harder than calcite.
Types:
Etymology:
Named after the French geologist Déodat Gratet de Dolomieu, who first described the mineral.
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Uses:
Distribution:
Found worldwide, especially in ancient marine environments
Historical Use:
Used in construction for thousands of years. The Dolomite Mountains in Italy are famous for their dolomite formations.
Symbolism:
Represents transformation and Earth's chemical processes
Dolomite contains magnesium (CaMg(CO₃)₂), while limestone is pure calcium carbonate (CaCO₃). Dolomite is harder and reacts less vigorously with acid.
Dolomite is found worldwide in ancient marine environments, especially in the Dolomite Mountains of Italy.
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