Crystal System: Calcite belongs to the trigonal crystal system, which means it has threefold symmetry.
Hardness: It has a hardness of 3 on the Mohs scale, which makes it relatively soft and easily scratched.
Color: Calcite can occur in a variety of colors, including colorless, white, yellow, orange, red, pink, blue, and green.
Transparency: It can be transparent to translucent, with a vitreous to resinous luster.
Cleavage: Calcite exhibits perfect rhombohedral cleavage, which means it can be broken into rhombohedral fragments.
Double Refraction: One of the most unique properties of calcite is its ability to exhibit double refraction, meaning it can split a single light ray into two rays.
Formation and Occurrence
Calcite forms in a variety of geologicalenvironments, including sedimentary, metamorphic, and igneous rocks. It is commonly found in limestone, marble, and chalk, as well as in hydrothermal veins and as a component of some igneous rocks.
Uses of Calcite
Calcite has numerous industrial and commercial uses, including:
Develop a model to illustrate that the release or absorption of energy from a chemical reaction system depends upon the changes in total bond energy.
Energy
Students who demonstrate understanding can:
Create a computational model to calculate the change in the energy of one component in a system when the change in energy of the other component(s) and energy flows in and out of the system are known.
Plan and conduct an investigation to provide evidence that the transfer of thermal energy when two components of different temperature are combined within a closed system results in a more uniform energy distribution among the components in the system (second law of thermodynamics).