$Calcite is one of the most common minerals on earth. It occurs in a seemingly unlimited variety of shapes and colors. It is a very important part of many of the rocks on Earth. Calcite belongs to the group of calcite minerals, a group of related carbonates that are isomorphic with others. They are similar in many physical properties, and can be partially or completely replaced with each other, forming a series of solid solution. All members of the calcite group crystallize in the trigonal system, have perfect rhombohedral cleavage, and exhibit strong double refraction in transparent rhombohedra.$

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