Mineral Structure Essay

700 Words2 Pages

Bonds and Properties in Mineral Structure A mineral is a naturally occurring, inorganic, homogeneous solid with a definite chemical composition and an ordered atomic arrangement(*). Despite the most minerals are chemical compound, some of them are elements such as Gold, Cupper, Sulfur. There are approximately 3000 minerals in the nature. The minerals separate from the each other with their specific chemical and atomic structure. They crystallize regularly in 3-Dimesions. When that happens, some forces bind together the atoms and lead to the formation of an aggregate as an independent molecular species. These forces are called the chemical bonds and they have four main types; covalent, ionic, …show more content…

It is most stable configuration for atom because the outer shell of the atom is completely filled. Minerals that contains covalent bonds are insoluble, stable, brittle and they have high melting points. The elements in the Carbon group like carbon, silicon, tin prefer covalent bonding. For instance, two Carbon atoms bond together with covalent bonding and that is the strongest bond in nature. (**) Secondly, the ionic bond involves transfer the electrons to achieve a completely filled outer shell. This type of bond occurs between metals and nonmetals. When the metals want to lose their electron, the nonmetals want to gain to achieve noble gas configuration. The crystals which have this type of bond, have hardness and specific gravity moderately. They have also high melting point and they are poor conductors. Bonding in most of the minerals is largely ionic. (***) Thirdly, in the metallic bond, electrons are free to float about the metal crystalline structure. This type of bond occurs only between metals like gold. The metals lose their other electrons easily. Because of the movement of the electrons, the minerals which have the metallic bond, conduct the electricity very well. The metallic bonding is seen in native mineral like Au, Ag, Cu(****). It is known that they have ductility and low …show more content…

We said that the minerals have crystalline structures in three dimensions. Some of these minerals have weak bonds in their structures. Because of the weakness, there is some fractions in their surfaces parallelly. This tendency of these minerals to break is called cleavage. The surfaces of the minerals which have cleavage, also have minimum cohesion. (*******) The another property is parting. The parting looks like the cleavage but not the same. The difference between cleavage and parting is that if the broken piece remains a crystal shape, this situation is called cleavage. However, when the parting occurs crystals divide in two. The fracture, on the other hand, occurs randomly because of the crest impact. (Sample of fracture) (********) Lastly, Hardness is the strength of the minerals. It is about the forces of the bonds between the atoms. Although some minerals are soft, some of them are very hard. For instance, the diamond is the hardest one but the talc is the

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