would be to identify calcite by use of double refraction. Light splits into two rays and undergoes twofold refraction when it passes through calcite. We can recognize calcite by these.
Marble and limestone are primarily composed of calcite. The Earth's crust is largely composed of these extremely common rocks. They are one of the world's largest carbon storage areas. Calcite is one of the most often utilised minerals due to its unique features. Although calcite reacts with HCl impressively, the main application of this reaction in the field is to distinguish between limestone and dolostone. My recommendation is to identify calcite by use of double refraction. When light travels through calcite, it is refracted twice.
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