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Magnesite
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The most common form of Magnesite is white, microcrystalline, porous masses that are dull in luster and have the appearance of unglazed porcelain. Magnesite belongs to the Calcite group of minerals, a group of related carbonates that are isomorphous with one another. They are similar in many physical properties, and may partially or fully replace one another, forming a solid solution series. All members of the Calcite group crystallize in the trigonal system, have perfect rhombohedral cleavage, and exhibit strong double refraction in transparent rhombohedrons.
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