Crude Perlit
Raw Perlite is a name given to naturally occurring silica-based volcanic rocks.
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Description
Raw Perlite is a name given to naturally occurring silica-based volcanic rocks. Due to the volcanic occurrence of all raw perlite occurrences; it is directly related to volcanic formation, relativism, mechanism and paleovolcanic evolution. Volcanoes are formed by the melting or insoluble matter in the ground, where the gases emerge from a weak zone (a slit or a hole). The volcano is formed by the upward movement of high pressure gases collected in the depths of the ground nightmare or under the shell. The magmatic masses carried by moving high pressure gases constitute the main material of the volcano. Perlite is found in these materials. The investigation of magmatic activities and their qualities and origins is the subject of volcanism and volcanology. Volcanic activity is related to the adhesive magma under the Sial Shell in the inner part of the globe, that is, to Sima and to a high temperature and pressure. On the one hand, the high temperature in the ground, on the other hand, from the bottom upwards to the surface of the high pressure effect of the stacked substances, their physical and chemical characters in terms of origin and location in the outer layer between the Sial shell and the center Nife part of the activities due to the inner layer.
The substances that come with volcanoes melted to the earth are collected from time to time in molten magma furnaces and pushed upwards. The magma movements of the volcanoes and the hearths erupt by dislocations under the crust and generally due to the movements in the earth's crust, and thus emerge from the weak playful places of the earth crust. The solids that come out in this blow and the semi-liquids which come with them, are absorbed into the air and out of the earth. Volcanic pines, such as perlite, are formed by the sudden cooling of the lava. The shafts and the break points are always bright. Their color varies according to the essential elements of their composition.
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