Earth And Space Science

Chapter 25 : Minerals and How We Use ThemElements combine together to miscellanea incompatible minerals and minerals combine to potpourri rocks . There ar 92 by nature occurring elements and with exception of a few inert elements alike(p) meretricious , Platinum etc , they combine together to form as some(prenominal) as 4000 minerals . Out of this large number of minerals only fair two dozens atomic number 18 habitual (constitutes 99 of priming crust ) and these be composed of about a dozen elements . These rock forming elements foundation be sort out in quintuplet groups - silicates carbonates , oxides and sulfates . In following sections we will soon describe these minerals , their defining and usageSilicates : Silicon is the 2nd most colossal element abutting to group O on the country crust . It combines w ith group O to form a tetragonal change SiO2 , which combines together to form a large tetragonal social organization Besides , SiO2 combines with other admixture oxides , to form their silicates Some examples of viridity silicates are Olivine , Pyroxene , Amphibole Micas , Feldspar etcCarbonates : Carbonates CO32- are linear molecules consisting of carbon and oxygen . These ions are arranged in the form of sheet in minerals like Calcite and DolomiteOxides : Metals react with oxygen to form their oxides . Some in-chief(postnominal) oxide minerals are Hematite (Fe2O3 , magnetite (Fe3O4 , Chromite (Cr2O3 , Cassiterite (SnO2 ) etcSulfides : These are alloy-sulfur compounds . Some big sulphide compounds are cognize as Pyrites like Chalcopyrite , Fools aureate etc . These minerals have gilded lusterSulfates : These are composed of metal ions and sulfate ions (SO42- These minerals have often no ore take to be to the conflict . However , these are employ as compounds . One i mportant sulfate mineral is Gypsum (CaSO4 .2! H2OMineral brass : Minerals form by quartz and growth in a liquid . The liquid can be either a molten rock or an aqueous solution When temperature of a molten rock or magma falls below freezing point of a mineral , the mineral crystallizes . Minerals do not have a sharply freezing point sort of they solidify over a range , dep balanceing on their theme .

The first to solidify is the 1 having highest curing point and this is lechatelierite , subsequently other metal silicates solidify . Minerals solidifying towards the end have lowest solidification pointBesides , minerals crystallize in aqueous solution as headspring . This happens when an aqueous solution having minerals at some temperature , becomes supersaturated repayable to change in temperature (generally change , but sometimes heat energy as sound . In case of mineral temerity from an aqueous solution , what is important is solubility and not the melting point of the mineralProperties of Mineral : Minerals are characterized by some of their ludicrous properties like Crystal form , clumsiness , Cleavage and shift key Color , Specific staidness etc . crystal form of a mineral depends on the sexual arrangement of the dower atoms / ions . This leads to well developed faces of the crystal and is a very important breath of crystal identification . Hardness of a mineral depends on the bond strength of the constituent atoms / ions . It is measured on Mohs eggshell (1 to 10 Higher Mohs value implies higher hardness 10 is for diamond...If you want to get a full essay, order it on our website: OrderEssay.net

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