Dolomite is a mineral composed of calcium and magnesium carbonate CaMg(CO3)2, in which there is a substitution by ionic exchange of calcium for magnesium in the limestone CaCO3.

At Sodira, the dolomitic mineral extracted at the Monda mine stands out for its exceptional characteristics, which, combined with the careful transformation and storage to which it is subjected in each of our processes, make it one of our reference materials.