Calcite is a common mineral composing such rocks as chalk and marble. It has the formulae CaCO3 and a relative hardness of 3. It effervesces vigorously with HCl. Clear specimens exhibit double refraction. Occurs as widespread sedimentary rock masses such as limestone. Crystalline metamorphosed limestones are called marbles. Argentine is a pearlylamellar variety; aphrite is foliated or chalklike; dogtooth spar, a form in acute rhombohedral or scalenohedral crystals; calc- sinter and calc-tufa are lose or porous varieties formed in caverns or wet grounds from calcareous deposits; agaric mineral is a soft, white friable variety of similar origin; stalactite and stalagmite are varieties formed from the drillings in caverns. Iceland spar is a transparent variety, exhibiting the strong double refraction of the species, and hence is called doubly refracting spar. Research Calcite
A stalactite is a mass of calcareous matter hanging in caves, formed by the filtration of water containing calcium bicarbonate in solution through holes or pores in the caveroof. the evaporation of the water and carbonic acid gas leaves behind it a deposit of limestone which continues to increase in size so long as the water drops. Research Stalactite
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Research Calcite
