Atacamite is one of the minerals which has a tendency of distribution in the desert areas.It was generally discovered in the Atacama Desert which is considered as the hardest areas in the world. This mineral was generally discovered in the year of 1801 in the Atacama area in the country of Chile. It can be sometimes referred to by the names likeAlacamite, Marcylite, Kupfert And or Arsenio (I, Dossett &D, I, Green, 1998).The mineral of Atacamite has one of the complex structures in nature. The structure ofAtacamite mineral can be described by characterizing both its physical and chemical structure. Atacamite mineral is a mineral which has the chemical formula of Cu2Cl (OH) 3.This mineral usually. This mineral is a halide which forms the natural salts. The atacamite is attractive in nature. This mineral is a polymorphic mineral which has the same chemistry with the botallackite and paratacamite. The color of the catamite is characterized by the shades of deep green color or black green. It has the cleavage which can be characterized as being perfect and that cleavage is of the size of 010. This mineral has the density of 3.76-3.78 with an average of 3.76.It is one of the mineral which has the diaphaneity ranging from transparent to transluncent. The fractures on it are characterized as being conchoidal in nature, which is the fractures are characterized by the smooth curves. The crystals of these minerals are composed of the mineral fibers. This mineral has been found to be generally occurring as cathedral crystals. In reference to its hardness, the atacamite has the degree of hardness which ranges from 3-3.5.The light characteristic of this mineral is that it’s a non-luminescent in nature. On the other hand this mineral has the apple green streak with the luster of adamantine. The mineral species which Occur in nature with this atacamite structure is copper which belongs to the halide group (N.J. Elton, 1998). This occurrence of the copper species has been attributed by the fact that atacamite minerals have an occurrence in the desert areas at the zone of the oxidized deposits of the copper mineral. At the other hand they are formed in the fumaroles deposits. On the other hand the atacamite minerals are regarded as the minerals which are formed by the oxidation of the copper minerals. Sometimes the atacamite has been considered as altered products of copper and bronze. The solid solution which occurs between the members of the atacamite mineral group is the oxy-halide in nature. It contains oxygen and hydroxides as their chemical composition. They are generally considered to be aqueous in nature (T. F. Bridges & B. Young, 1998) The techniques which are used to analyze the composition of the atacamite structure vary from one analytical laboratory to another. The mostly commonly used methods include the use of the photographic light polarizing microscopy, radioactivity techniques, spectroscopic techniques, Mohs scale method and the crystallization technique. In the technique of the microscopy the atacamite minerals are observed as having crystals with the bright greenish or the blackish greenish colour. At the same time this mineral shows displays which are vi