Dolomite from Horsmanaho, Finland.
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Dolomite from Innansjön.
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| Mineral class | Carbonates, dolomite-ankerite group. |
| Chemical formula | CaMg(CO3)2 |
| Crystal system | Trigonal |
| Habitus | Romboedric crystals with curved surfaces {10/11}. Also as grainy masses. |
| Hardness | 3.5-4 |
| Density | 2.8-2.9 |
| Color | usually colorless, but nuances in yellow, gray and pink. |
| Luster | glas to pearly. |
| Description | Dolomite is usually created through metasomatic transformation
of calcite under appending of magnesium ions. Dolomite can also be created through hydrothermal transformation of magnesium rich carbonate and silicate rocks. Together with dolomite, magnesite, serpentine, brucite and magnetite are also created. (As in Modum) |
| Occurance | Dolomite is the main ingredience of dolomitic marble. It can also occur in hydrothermal veins, around mangane mines, and in some serpentinites. |
| Associates | calcite, magnesite, serpentine, brucite, magnetite |
| Notes | Dissolves slowly in cold hydrochloric acid, fast only as a
pulver or in hot acid. Named after the French geologist D Dolomieu (1750-1801). |
| Locations | Dolomite is a common mineral in Sweden, often around ores as
grainy masses. At some places as marble.
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| To carbonate index. |
Mineral group index. |
Main index. |
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