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Dolomite is a medium-value and economic type of sedimentary stone that forms entire layers. It is also a flux stone, meaning it can be used in the production of pig iron and steel. Additionally, it is magma safe, with an extremely high melting point of . It is pale pink with premium graphics or white with classic graphics.
Because of its abundance and utility, dolomite is one of the most remarkable non-ore stones, and is much more useful than many other flux stones.
Dolomite is slightly denser than the average rock, inhibiting hauling. Because of its status as a flux stone, which are in high demand in steel-making, wheelbarrows are useful for the transport of dolomite.
In real life
Dolomite is comprised of calcium magnesium carbonate (CaMg(CO3)2) and is related to limestone, chalk, and marble. Its ionic and crystalline nature contributes to its high melting point. It's dolomite, baby!
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Some Iron men have claimed that they are composed of 40% dolomite. However Iron men are known to frequently make illogical and exaggerated claims about their composition, especially ones whose internal mechanisms are powered by alcohol. As dolomite is magma-safe, it is sometimes touted that it "won't cop out when the heat's all about".
[INORGANIC:DOLOMITE] [USE_MATERIAL_TEMPLATE:STONE_TEMPLATE] [STATE_NAME_ADJ:ALL_SOLID:dolomite][DISPLAY_COLOR:7:7:1][TILE:'`'] [REACTION_CLASS:FLUX] not CaCO3, has Mg, makes "calcined dolomite" in calcination instead of quicklime, not sure of effective differences [SEDIMENTARY] [MATERIAL_VALUE:2] [IS_STONE] [MELTING_POINT:16507] [BOILING_POINT:18000] [SOLID_DENSITY:2850] [STATE_COLOR:ALL_SOLID:PALE_PINK]
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